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The Pelagic Environment of the Arabian Gulf

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ECOSYSTEMS AND BIODIVERSITY
OF THE ARABIAN GULF
SAUDI ARABIAN WATERS
Fifty Years of Scientic Research
A Publication by Saudi Aramco and King Fahd University of Petroleum & Minerals
Chief Editors
Dr. Khaled A. Al-Abdulkader1, Dr. Ronald A. Loughland1 and Dr. Mohammed A. Qurban2
1Environmental Protection Department, Saudi Aramco
2Center for Environment & Water, King Fahd University of Petroleum & Minerals
Photography
Applaudo Grupa d.o.o.
Maps Production
Syed Azher Hussain
Publishing Coordination
Meerja Humayun Baig
Production and Direction
Bruno Nicolis
Design and Layout
Roberto Chillon
Printing and Binding
Papergraf - Piazzola sul Brenta (Padova), Italy
© 2019 Saudi Aramco & King Fahd University of Petroleum & Minerals
All right reserved. No part of this publication may be reproduced, stored in a retrieval system or
transmitted in any form or by any means, electronic, mechanical, photocopying, recording or
otherwise, except brief extracts for the purpose of review, without the prior permission in
writing of Saudi Aramco.
ISBN: 978-603-02-7862-6
Dr. KhaleD a. al-abDulKaDer, Dr. ronalD a. loughlanD, and Dr. MohaMMeD a. Qurban
ECOSYSTEMS
AND BIODIVERSITY OF
THE ARABIAN GULF
SAUDI ARABIAN WATERS
Fifty Years of Scientic Research
5
Preface
For nearly ve decades, the King Fahd University of Petroleum and Minerals (KFUPM) has partnered
with Saudi Aramco to document and explore the wondrous ecosystem that exists in the Arabian Gulf.
The book before you oers a comprehensive and up to date guide on the fruits of that work and its
ndings.
Through its pages, marine scientists, decision makers, students and indeed anyone with an interest in
marine environmental protection, will have access to a wealth of scientic information.
The Arabian Gulf is environmentally challenged because of the natural stressors of salinity and temperature
uctuations. Rapid population growth and associated developmental activities along its coasts, particularly
those related to the urban and industrial development, are adding additional stress on the Arabian Gulf s
fragile environment.
The partnership between KFUPM and Saudi Aramco, has resulted in a greater understanding of the
Arabian Gulfs natural ecosystems, ensuring greater protection of biodiversity and natural resources. The
backbone of this partnership has been the Marine Environmental Sustaining Research Program, which has
produced fundamental knowledge on the Arabian Gulf s marine environment. In addition, detailed and
in-depth environmental impact assessments have been systematically conducted for proposed development
projects as well as environmental monitoring during construction and commencement of operations, all
contributing to our knowledge of the ecosystems. This information has contributed to the protection of the
ecosystems and the development of a sheries management framework in the Arabian Gulf.
We are grateful for the collaboration and eorts of the interdisciplinary teams of the Environmental
Protection Department of Saudi Aramco and the Marine Studies Section of KFUPM in preparation of this
book. A deep and sincere appreciation is extended to each and every person who, for nearly ve decades,
has played a part in this partnership in marine environment protection. This book is a testament to your hard
work and our collective desire to preserve the beautiful ecosystem that ourishes in the Arabian Gulf.
A H. N
Saudi Aramco President & CEO
7
Foreword
The Arabian Gulf has always been a special component of the Kingdom’s economy and culture.
Aside from its rich oil and gas resources, it is also an important source of food and water, and
is a major transportation point. But not to be undermined or forgotten is the fact that it also
supports vital and thriving ecosystems. In its waters are seagrass, coral reefs, salt marshes, and mangroves,
as well as intertidal and subtidal sediments and deeper water areas. These interacting habitats provide the
essential components for a vibrant and productive marine ecosystem. However impressive this may sound,
the Arabian Gulf is also facing natural and human-induced stress, such as elevated seawater temperature and
salinity; coupled with coastal urbanization and rapid industrialization. These stresses, if not managed, can
impact the long-term ecosystem services currently provided by the Arabian Gulf.
Scientic research on its marine environment is the result of collaboration between industry and
academia. It was in 1982 that the Environmental Protection Department of Saudi Aramco and the Marine
Studies Section of the King Fahd University of Petroleum and Minerals began joint research into the
Arabian Gulfs ecosystem. This partnership involved the development of research programs to study the
Arabian Gulfs ecosystem values, interactions, and reduce the impact of stress. Currently, the sixth phase of
this sustaining research program is focusing on the biodiversity status across the Arabian Gulf s ecosystems.
This book gathers the results and the major scientic ndings of this long-term collaborative program and
provides a detailed, updated review on the state of the marine ecosystems and biodiversity of the Western
Arabian Gulf. For anyone who has an interest in the topic, it serves as the current denitive work, and is a
reminder of the importance of marine ecosystems.
P. S N. A
Rector of King Fahd University
of Petroleum & Minerals
Chapter Three
The Natural Ecosystem
of the Western Arabian Gulf
Chapter One
General Introduction
Preface
Foreword
Contents
7
9
Chapter Two
The Phisical Environment
of the Western Arabian Gulf
Chapter Four
Fauna
19
61
11
325
Chapter Six
Impacts on Ecosystems:
Mitigation and Management
Chapter Seven
Management of the Gulfs
Ecosystems: The Way Forward
Chapter Five
Use of the Natural Resources
References
Appendix
451
515
547
616
569
309
THE NATURAL ECOSYSTEMS OF THE WESTERN ARABIAN GULF
3 .11
The Pelagic Environment
of the Arabian Gulf
Todd r. Clardy1, MoriTz J. Heinle1, and yu-Jia lin1
Introduction
The marine pelagic ecosystem is dened as the portion of the ocean that is not inuenced by the
ocean bottom or by coastal eects, such as freshwater discharge from rivers or anthropogenic wastewater
discharge. This makes the marine pelagic realm the largest ecosystem on Earth. Oceans cover 71% of the
Earth’s surface and have an average depth of 3.8 km, meaning approximately 99% of Earth’s available livable
habitat is the pelagic realm (Norse, 1994). Due in part to its large size, the pelagic environment directly
or indirectly inuences almost all marine life and has a major inuence on terrestrial life as well. Pelagic
waters account for a large proportion of primary production on Earth (Field, et al., 1998) and provide
> 80% of the sh consumed by humans (Pauly, et al., 2002). Given their size and importance, marine
pelagic ecosystems have been well studied globally, including their biodiversity, trophic structure, nutrient
cycling, response to climate change, and more.
Pelagic waters are divided into zones depending on light availability and water depth (Walker and
Wood, 2005). The epipelagic zone encompasses the upper 200 m of oceanic waters and is the region
where sunlight is most abundant and primary production is highest. Between 200 m to 1,000 m is the
mesopelagic zone, where light is available but is generally too diuse to support primary production.
Below 1,000 m is the bathypelagic zone, which is the region beyond sunlight penetration.
The entire basin of the Arabian Gulf (hereafter “Gulf”) is less than 100 m deep, and as a result, all
pelagic waters of the Gulf are considered epipelagic. The epipelagic realm in the Gulf covers an extensive
area in the central and eastern portions, but is limited along the western Gulf (Figure 3.109). Along the
Arabian Peninsula, shallow waters of less than 20 m extend over 100 km from shore. There is a high
likelihood for interaction between the bottom and the water column in these shallow regions, and for the
purposes of this chapter, they are not considered truly pelagic.
The pelagic realm is one of the largest and most important ecosystems in the Gulf. The arid climate
of the Middle East and high levels of photosynthetically active radiation promote a rich phytoplankton
assemblage and high primary production. This, in turn, supports a rich zooplankton and pelagic sh
community. Every nation in the Gulf has pelagic waters in its Exclusive Economic Zone, except Iraq
whose Gulf access is conned to the Shatt Al-Arab estuary. Given the ecological and economic importance
1
Center for Environment & Water, Research Institute, King Fahd University of Petroleum & Minerals, Dhahran, Kingdom of Saudi Arabia.
Email: tclardy@kfupm.edu.sa.
310
CHAPTER 3
Figure 3.109. The Arabian Gulf. The red line indicates the 20 m isobath.
of pelagic waters to the region, an understanding of pelagic ecology is essential to successful management
of pelagic resources by all nations in the Gulf.
Distribution
The Gulf has a surface area of approximately 2.39 × 105 km2 but a volume of just 8.63 × 105 km3
(Reynolds, 1993). The deepest waters, about 100 m, are found in a trough of water that extends northwest
along the coast of Iran from the Strait of Hormuz where the Gulf opens into the Gulf of Oman (Reynolds,
1993). Most of the Gulf is less than 60 m, and the average depth is just 35 m.
The Gulf lacks signicant riverine discharge or other coastal inputs for most of its coast. Only six
major rivers discharge into the Gulf, providing minimal freshwater input. Three of these rivers, the Tigris,
Euphrates, and Karun, discharge into the Shatt Al-Arab estuary in the northwest portion of the Gulf,
forming a complex oodplain estuary. In Iran, the Hendijan, Hileh, and Mand rivers provide additional
311
THE NATURAL ECOSYSTEMS OF THE WESTERN ARABIAN GULF
sources of freshwater input. Collectively, these rivers discharge 3,490 m3/s of freshwater into the Gulf
(Reynolds, 1993). The remaining areas of the Gulf, particularly those on the southwestern coast, lack
substantial riverine input. No major rivers discharge from Saudi Arabia into the Gulf.
The shallow depth of marine waters in the western Gulf limits the area of pelagic habitat of Saudi
Arabia. Much of Saudi Arabian waters are shallower than 20 m, and extensive areas are less than 10 m.
Pelagic waters are found primarily in the northeastern region where a deep trough of water extends
southeast from Kuwait to the central point of the Saudi coastline around Al-Jubail. Southeast of Al-Jubail,
the depth decreases to less than 20 m with only small pockets of deeper water. All waters southwest of
Dammam, including those that border Bahrain and Qatar, are shallower than 10 m.
Chemical Oceanography
Salinity in pelagic waters of the Gulf ranges from 35 psu to 43 psu, with a trend for increasing salinities
north to south (KFUPM/RI, 2006a). In Saudi waters of the Gulf during the spring, surface waters become
less saline than deeper waters due to surface currents, supporting the development of the pycnocline.
An important regulator of seawater chemistry is pH, which aects properties of chemical compounds,
such as chemical reactions or equilibrium conditions. In the Saudi pelagic waters of the Gulf, the pH
range is 7.39 to 8.32, with a clear annual cycle (KFUPM/RI, 2006b). The highest pH is observed during
the winter, after which it continuously declines toward the summer and starts to increase again in the fall.
This is a result of the temperature eect on pH, in which an increase in temperature leads to an increased
production of H+, and therefore, a decrease in pH.
Another important parameter in seawater chemistry is the concentration of dissolved oxygen (DO),
because it provides indications on primary production and the potential for secondary consumers to live in
an area. DO in the pelagic zone of the Gulf varied from 0.81 mg/l to 9.37 mg/l during a study in 2002 and
2003, corresponding to an oxygen saturation of the water of 11.7% to 135.5% (KFUPM/RI, 2006a). DO
shows a clear annual cycle with maximum concentrations during the winter and minimum concentrations
during the summer, resulting from higher water temperatures during the summer and corresponding
lower solubility of oxygen. Additionally, stratication leads to vertical dierences in concentration during
the summer, with higher levels in surface waters than in deeper waters (KFUPM/RI, 2006b).
Nitrogen, primarily in the form of nitrite (NO3), nitrate (NO2), and ammonia (NH4), and phosphorous,
primarily as phosphate (PO4), are important elements for primary production. Nitrite concentrations in
the pelagic zone of the Arabian Gulf ranged from 0.86 µg/l to 42.21 µg/l, nitrate from 1.7 µg/l to 521.78
µg/l, and phosphate from 0.42 µg/l to 349.07 µg/l in a 2002 and 2003 study (KFUPM/RI, 2006a). These
concentrations are within the range of two other studies that studied the pelagic ecosystem in the Arabian
Gulf (Hashimoto, et al., 1998; ROPME, 2012). Deep waters in the pelagic zone have higher concentrations
of nitrate and nitrite than surface waters, although no such trend is found for phosphate. These dierences
were most pronounced during the spring and summer, indicating that Gulf deepwater is richer in nitrogen
compounds than the Indian Ocean surface water. Maximum concentrations were found at the onset of
summer (nitrite and nitrate) and spring (phosphate), whereas minimum concentrations were measured
312
CHAPTER 3
during the fall (nitrite) and winter (nitrate and phosphate). This results from increased biological activity
during the summer. For the whole Gulf, nutrient concentration decreases in a south-north direction,
as inowing water from the Strait of Hormuz enters the Gulf and nutrients are continuously used by
phytoplankton (ROPME, 2012). Common values of abiotic parameters are shown in Table 3.34.
Phytoplankton
The phytoplankton community in pelagic waters of the Gulf is dominated by diatoms (83% of all species)
with dinoagellates (15% of all species) the second most species rich group (Dorgham, 2013). At least 1,114
phytoplankton species have been identied from the Gulf, 888 of which are diatoms (Dorgham, 2013). In
an extensive cruise during the 2006 winter, it was found that phytoplankton species diversity decreased
noticeably with depth (ROPME, 2012). This study found a higher contribution of dinoagellate species (55%)
than diatom species (42%) to the overall community. This is in contrast to the review by Dorgham (2013)
and indicates variation in the contribution of these two important groups of phytoplankton. The ROPME
(2012) study also observed signicant dierences in community composition between the inner Gulf and the
Gulf of Oman, resulting from two currents that form two frontal zones in the western and eastern Gulf from
freshwater input from Shatt Al-Arab and inow from the Arabian Sea via the Gulf of Oman.
Most phytoplankton studies in waters of Saudi Arabia have focused on nearshore waters, which are
inuenced by shallow depth and nutrient input from land, and therefore, not considered pelagic. Only
one study in Saudi waters included stations that can be considered truly pelagic (KFUPM/RI, 2006c). In
general, the phytoplankton community in the Arabian Gulf is dominated by diatoms and dinoagellates
(Dorgham, 2013). In a study conducted by the King Fahd University of Petroleum and Minerals Research
Institute (KFUPM/RI) during 2002 and 2003, the phytoplankton community in all Saudi waters of the
Gulf was dominated by diatoms (65% of all species), followed by dinoagellates (30% of all species), but with
noticeable annual variability (KFUPM/RI, 2006c). Maximum cell concentrations were observed during
the summer with a second, smaller peak in the winter. Subsequently, species diversity was considerably
Table 3.34. Abiotic parameters in the pelagic waters of the Arabian Gulf.
Parameter Low High Source
Temperature 14°C 35°C Reynolds (1993)
Salinity 35 psu 43 psu KFUPM/RI (2006a)
pH 7.39 8.32 KFUPM/RI (2006b)
DO concentration 0.81 mg/l 9.37 mg/l KFUPM/RI (2006a)
DO saturation 11.7% 135.5% KFUPM/RI (2006a)
Nitrite 0.86 µg/l 42.21 µg/l KFUPM/RI (2006a)
Nitrate 1.7 µg/l 521.8 µg/l KFUPM/RI (2006a)
Phosphate 0.42 µg/l 349.07 µg/l KFUPM/RI (2006a)
313
THE NATURAL ECOSYSTEMS OF THE WESTERN ARABIAN GULF
higher during the winter, because the community was dominated by a small number of species with high
cell concentrations during the summer (46% Trichodesmium erythraeum and 25% Thalassionema nitzschoides
during the 2003 summer), whereas it was more evenly distributed during the winter (21% Chaetoceros
curvisetus, 19% Laudaria annulata, 18% Thalassiosira subtilis, 16% Thalassionema nitzschoides during the 2003
winter). This results from higher nutrient concentrations during the summer, which enables fast-growing
species with high nutrient demands to dominate the community. During the winter, nutrients are still being
replenished, and concentrations are lower, which allows a wider variety of phytoplankton species to grow.
During the fall, cell concentrations decline as nutrients are depleted. At the same time, species richness
increases as species that dominate the summer phytoplankton cannot sustain growth any longer, leading
to a larger number of species with lower nutrient demands. During the spring, cell numbers decrease,
although nutrient concentrations continue to increase. This is likely an adaption of the phytoplankton
community to stratication, which develops during this season and persists until the end of the summer.
During this time, the majority of the phytoplankton community is found below the pycnocline where
enough light is available for photosynthesis and nutrient concentrations are considerably higher than in
surface waters. Light levels below the pycnocline might not yet be high enough during the spring to
support high phytoplankton growth rates, and plankton trapped below it cannot sustain high cell numbers.
The photosynthetic pigment chlorophyll a is an important parameter to characterize the phytoplankton
community, and chlorophyll a concentration is frequently used as proxy for primary production. Throughout
the Gulf, maximum concentrations of chlorophyll a are observed o Iran (3 mg/m3), corresponding to high
nutrient concentrations along the northeast coast (Hashimoto, et al., 1998; ROPME, 2012). Chlorophyll a
concentrations decrease from north to south in the pelagic realm of the Gulf. Concentrations in the Strait
of Hormuz and the adjacent Sea of Oman are often higher than within the Gulf, a result of intrusion of
water from the Gulf of Oman (ROPME, 2012). Seasonally, higher concentrations are observed during the
winter than in the summer (ROPME, 2012). Chlorophyll a concentration decreases with depth and is
negatively correlated with temperature and salinity (Hashimoto, et al., 1998; ROPME, 2012). Chlorophyll
a concentrations can be derived from satellite images, based on reectance of light at certain wavelengths.
In general, satellite estimates of chlorophyll a concentrations are most eective in pelagic ocean waters and
often overestimate concentrations in shallow, turbid areas. Subsequently, eld and laboratory measurements
in the Gulf have found good agreement with data from the MODIS satellite (ROPME, 2012). A two-
year study of satellite images in the Gulf indicates a decreasing gradient in chlorophyll a concentration
throughout the year with persistent seasonal and spatial chlorophyll a concentrations (ROPME, 2012).
In a KFUPM/RI (2006c) study of chlorophyll a in Saudi waters of the Gulf, concentrations of chlorophyll
a ranged from 0.23 mg/m3 to 1.75 mg/m3 and mean concentrations increased throughout the year, reaching
its maximum in winter. This indicates that the maximum value in cell concentrations, observed during the
summer, mainly included small, fast-growing phytoplankton with lower cellular chlorophyll a concentrations.
Concentrations were within the range (0.06 mg/m3 to 10.08 mg/m3) found in other studies of the pelagic Gulf
(Hashimoto, et al., 1998; ROPME, 2012). During the fall and winter, maximum chlorophyll a concentrations
were measured in the surface waters, whereas during the spring and summer, maximum concentrations
occurred at a depth of 25 m to 30 m, below the thermocline, which indicates that phytoplankton biomass
is higher in the Gulfs deepwater than in the intruding Indian Ocean surface water. Compared with the
coastal environment, the pelagic zone usually shows lower chlorophyll concentrations, due to lower nutrient
concentrations (Hashimoto, et al., 1998; KFUPM/RI, 2006b, 2006c).
314
CHAPTER 3
Zooplankton
Zooplankton research in the Gulf dates back to the early 20th century when Pesta (1911) described a
new species of copepod from near the coast of Iran. Since that time, there have been numerous zooplankton
studies in the Gulf, the majority of which have focused on coastal habitats. The zooplankton studies of the
pelagic realm in the Gulf are restricted to a few Gulf-wide investigations or stem from coastal investigations
that also included a few pelagic stations. Several studies focused on the ecology of the Indian Ocean in
the 1960s included stations within the Gulf (Frontier, 1963; Fenaux, 1973; Kimor, 1973; Nellen, 1973).
These studies provided important snapshots into the diversity and distribution of pelagic zooplankton
communities in the Gulf. These early investigations generally represented single cruises spaced out over
months or years, focused on individual groups of organisms, or had fewer than a dozen pelagic sampling
stations.
Later Gulf-wide studies investigated pelagic zooplankton at a higher resolution than these early eorts.
Between September 1979 and August 1980, the Kuwait Institute of Scientic Research conducted a series
of cruises in the western and southern Arabian Gulf (Houde, et al., 1986; Michel, et al., 1986a, 1986b).
Most of the eort was focused on 19 stations in Kuwaiti waters, ve of which were pelagic. A single cruise
between February and March 1980 sampled at 54 stations in waters from Kuwait to the Strait of Hormuz,
26 of which were pelagic. Pelagic zooplankton communities were dominated by copepods and nauplii
over 60% of total zooplankton abundance followed by gastropods and larvaceans (Al-Yamani, et al., 1993,
1998; Al-Khabbaz and Fahmi, 1998). Following the Gulf War, a series of cruises were conducted by the
Regional Organization for the Protection of the Marine Environment (ROPME), a group comprised of
all nations bordering the Arabian Gulf, in the western Arabian Gulf to assess the eects of a 6 to 8 million
barrel oil spill discharged during the conict. Zooplankton collections were made in the summer 2000 and
2001 and the winter of 2006. These cruises collected zooplankton from dozens of stations in the western
and central Gulf, over half of which were in the pelagic realm (ROPME, 2012). These surveys found patchy
distributions of zooplankton throughout the Arabian Gulf with no clear biogeographic patterns. Pelagic
samples typically were dominated by copepods and naupli, which averaged 41% of the total abundance, but
locally accounted for up to 86% of the total abundance (ROPME, 2012). Other important zooplankton
groups include Hydromedusae, Siphonophora, Thaliaceae, and Polychaeta. A winter 2006 ROPME survey
collected zooplankton at 115 stations throughout the Gulf, including 69 in pelagic waters (Dorgham, et
al., 2008). From this survey, 210 species of zooplankton were identied in the Gulf (ROPME, 2012). Up
to 116 of these taxa were new, indicating a high potential for endemism in Gulf pelagic waters (ROPME,
2012). Zooplankton communities had the highest abundance and diversity near the Strait of Hormuz and
in a small coastal region near the border of Kuwait and Saudi Arabia.
Several of the Gulf-wide zooplankton surveys sampled within Saudi Arabian waters (Kimor, 1973;
Michel, et al., 1986b; Al-Yamani, et al., 1993; Dorgham, et al., 2008), and numerous others have focused
exclusively on zooplankton within Saudi waters (Price, et al., 1993; KFUPM/RI, 1990; Azis, et al., 2003;
Baker and Hosny, 2005). The majority of these studies focused exclusively on coastal waters, such as within
Tarut Bay (KFUPM/RI, 1990) and Half Moon Bay (Baker and Hosny, 2005), and near desalination plants
(Azis, et al., 2003), meaning relatively little eort has been dedicated to pelagic waters. Moreover, these
studies focused on particular components of the zooplankton community, such as decapod larvae, and used
dierent sampling equipment, making direct comparisons among the studies dicult. Nevertheless, several
315
THE NATURAL ECOSYSTEMS OF THE WESTERN ARABIAN GULF
general trends in the pelagic zooplankton community can be identied from the collective research eort
in Saudi Arabian waters.
The composition of pelagic zooplankton communities in the Saudi Arabian waters of the Gulf reects
the general trends in the entire Gulf in that they are dominated by copepods, which can account for up to
85% of the total zooplankton abundance and frequently account for over 60%. From six samples collected in
Saudi waters in December 1994, Al-Khabbaz and Fahmi (1998) noted that cyclopoid and calanoid copepods
were nearly equally abundant with the cyclopoid genera Oithona and Oncea in the highest densities followed
by the calanoid genera Acartia and Paracalanus. A total of 21 copepod genera have been identied from Saudi
pelagic waters, though the number of genera is likely much higher and the number of species is unknown.
Generally, the diversity of copepods is equal to that of other regions of the Gulf (Al-Khabbaz and Fahmi, 1998),
although the densities are lower. For example, Al-Khabbaz and Fahmi (1998) found the total copepod density
to be 1,295 individuals/m3, while densities o Bahrain (2,963 individuals/m3), Qatar (4,633 individuals/m3),
and the United Arab Emirates (UAE) (6,333 individuals/m3) all were signicantly higher. After copepods,
gastropods, larvaceans, and ostracods are frequently the dominant groups, although, individually, these groups
make up less than 15% of the total zooplankton abundance (Michel, et al., 1986b; Al-Yamani, et al., 1998).
Groups such as decapods, chaetognaths, polychaetes, and larval shes make up a relatively small percentage of
the overall zooplankton community, usually less than 5%.
Biodiversity of pelagic zooplankton is often lower in waters of the Gulf than in surrounding regions. For
example, euphausids (Weigmann, 1970), appendicularians (Fenaux, 1973; Yamazi, 1974), and chaetognaths
(Furnestin and Codaccioni, 1968; Yamazi, 1974) each have a higher species count in the Arabian Sea, Indian
Ocean, and Red Sea than they do in the Arabian Gulf. This is likely a consequence of the shallow, warm,
saline waters of the Gulf, which selects for zooplankton adapted to the epipelagic realm. The waters of the
Arabian Sea, Indian Ocean, and Red Sea extend to the mesopelagic and bathypelagic realms, potentially
leading to greater biodiversity. Many zooplankton communities have a vertical component, and many
species utilize diurnal vertical migration, wherein they reside at the surface during the night and migrate
to deeper depths during the day. Many species are also adapted to low-light conditions in the mesopelagic
realm. Given the shallowness of the Gulf, it is unlikely that organisms adapted for a depth strata deeper than
100 m or those that experience diurnal vertical migration can survive in the Gulf.
Fishes
At least 101 species of shes in the Arabian Gulf live predominantly in the pelagic realm, many of
which support valuable sheries throughout the region (Table 3.35). Many other species make occasional
use of pelagic waters for feeding, transport, or reproduction, but are more often associated with demersal
habitats.
Ecological studies on pelagic shes in the Gulf have been limited. One of the most comprehensive was
carried out by the United Nations Food and Agriculture Organization in the late 1970s (Junemann, et
al., 1981). This survey, primarily conducted o the coast of the UAE, used a mix of acoustic sonar, gillnet,
purse seine, and trolling surveys to characterize pelagic sh communities in the southeastern Gulf. From
these surveys, the Sind sardine Sardinella sinensis was the dominant species (up to 90% of the total catch),
316
CHAPTER 3
Table 3.35.
Pelagic fishes of the Arabian Gulf, based on Carpenter, et al. (1996) and data from the KFUPM Fishery Program.
Taxa with asterisks indicate species with taxonomic confusion that are difficult to distinguish from other species.
Family Genus Species Common Name Presence in
Saudi Arabia
Rhincodontidae Rhincodon typus Whale shark Rare
Carcharhinidae Carcharhinus amblyrhynchoides Blacktail reef shark Rare
Carcharhinidae Carcharhinus limbatus Blacktip shark Rare
Carcharhinidae Carcharhinus plumbeus Sandbar shark Rare
Carcharhinidae Galeocerdo cuvier Tiger shark Rare
Carcharhinidae Rhizoprionodon acutus Milk shark Occasional
Carcharhinidae Rhizoprionodon oligolinx Grey sharpnose shark Rare
Sphyrnidae Sphyrna lewini Scalloped hammerhead Occasional
Sphyrnidae Sphyrna mokarran Great hammerhead Rare
Sphyrnidae Sphyrna zygaena Smooth hammerhead Rare
Myliobatidae Aetobatus narinari Spotted eagle ray Rare
Myliobatidae Aetomylaeus maculatus Mottled eagle ray Rare
Myliobatidae Aetomylaeus niehofii Banded eagle ray Frequent
Mobulidae Mobula diabolus Devil ray Rare
Clupeidae Hilsa kelee Kelee shad Rare
Clupeidae Tenualosa ilisha Hilsa shad Occasional
Clupeidae Amblygaster sirm Spotted sardinella Occasional
Clupeidae Herklotsichthys lossei Gulf herring Occasional
Clupeidae Herklotsichthys quadrimaculatus Bluestripe herring Frequent
Clupeidae Sardinella albella White sardinella Occasional
Clupeidae Sardinella gibbosa Goldstripe sardinella Frequent
Clupeidae Sardinella longiceps Indian oil sardine Frequent
Clupeidae Sardinella melanura Blacktip sardinella Occasional
Clupeidae Sardinella sindensis Sind sardinella Rare*
Clupeidae Anodontostoma chacunda Chacunda gizzard shad Not recorded
Clupeidae Nematalosa nasus Bloch’s gizzard shad Frequent
Clupeidae Nematalosa persara Persara gizzard shad Rare*
Clupeidae Nematalosa resticularia Gulf gizzard shad Rare*
Clupeidae Dussumieria acuta Rainbow sardine Not recorded
Clupeidae Dussumieria elopsoides Slender rainbow sardine Not recorded
Clupeidae Etrumeus teres Redeye round herring Not recorded
Clupeidae Spratelloides delicatulus Delicate round herring Not recorded
Pristigasteridae Ilisha compressa Compressed ilisha Rare*
Pristigasteridae Ilisha melastoma Indian ilisha Occasional
Pristigasteridae Ilisha sirishai Lobejaw ilisha Not recorded
Engraulidae Encrasicholina devisi Devis’ anchovy Rare*
Engraulidae Encrasicholina heteroloba Shorthead anchovy Rare*
Engraulidae Encrasicholina punctifer Buccaneer anchovy Frequent
Engraulidae Stolephorus indicus Indian anchovy Frequent
Engraulidae Stolephorus insularis Hardenberg’s anchovy Rare*
Engraulidae Thryssa baelama Baelama anchovy Not recorded
Engraulidae Thryssa dussumieri Dussumier’s thryssa Occasional
317
THE NATURAL ECOSYSTEMS OF THE WESTERN ARABIAN GULF
Family Genus Species Common Name Presence in
Saudi Arabia
Engraulidae Thryssa hamiltonii Hamilton’s thryssa Occasional
Engraulidae Thryssa vitrirostris Orangemouth anchovy Not recorded
Engraulidae Thryssa whiteheadi Whitehead’s thryssa Not recorded
Chirocentridae Chirocentrus dorab Dorab wolf-herring Frequent
Chirocentridae Chirocentrus nudus Whitefin wolf-herring Frequent
Bregmacerotidae Bregmaceros nectabanus Codlet Rare
Bregmacerotidae Bregmaceros rarisquamosus Codlet Not recorded
Belonidae Ablennes hians Flat needlefish Frequent
Belonidae Platybelone argalus Keeltail needlefish Not recorded
Belonidae Strongylura leiura Banded needlefish Not recorded
Belonidae Strongylura strongylura Spottail needlefish Not recorded
Belonidae Tylosurus crocodilus Hound needlefish Frequent
Exocoetidae Cypselurus oligolepis Largescale flyingfish Rare
Exocoetidae Parexocoetus mento African sailfin flyingfish Rare
Hemiramphidae Hemiramphus marginatus Yellowtip halfbeak Occasional
Hemiramphidae Hyporhamphus limbatus Congaturi halfbeak Rare*
Hemiramphidae Hyporhamphus sindensis Sind halfbeak Rare*
Hemiramphidae Hyporhamphus unicuspis Onecusp halfbeak Rare*
Hemiramphidae Rhynchorhamphus georgii George’s halfbeak Rare*
Rachycentridae Rachycentron canadum Cobia Occasional
Echeneidae Echeneis naucrates Sharksucker Occasional
Carangidae Atule mate Yellowtail scad Occasional
Carangidae Decapterus macarellus Mackerel scad Rare
Carangidae Decapterus russelli Indian scad Frequent
Carangidae Elagatis bipinnulata Rainbow runner Rare
Carangidae Megalaspis cordyla Torpedo scad Frequent
Carangidae Naucrates ductor Pilotfish Occasional
Carangidae Parastromateus niger Black pomfret Occasional
Carangidae Scomberoides commersonnianus Talang queenfish Frequent
Carangidae Scomberoides lysan Doublespotted queenfish Frequent
Carangidae Scomberoides tol Needlescaled queenfish Frequent
Carangidae Selar crumenophthalmus Bigeye scad Frequent
Carangidae Selaroides leptolepis Yellowstripe scad Frequent
Carangidae Seriola dumerili Seriola dumerili Occasional
Carangidae Trachurus indicus Arabian scad Frequent
Carangidae Uraspis helvola Whitetongue jack Rare*
Coryphaenidae Coryphaena hippurus Common dolphinfish Occasional
Sphyraenidae Sphyraena barracuda Great barracuda Not recorded
Sphyraenidae Sphyraena flavicauda Yellowtail barracuda Occasional
Sphyraenidae Sphyraena forsteri Bigeye barracuda Frequent
Sphyraenidae Sphyraena jello Pickhandle barracuda Occasional
Sphyraenidae Sphyraena obtusata Obtuse barracuda Frequent
Sphyraenidae Sphyraena putnamae Sawtooth barracuda Frequent
Sphyraenidae Sphyraena qenie Blacktail barracuda Occasional
Scombridae Auxis rochei Bullet tuna Not recorded
318
CHAPTER 3
with the rainbow sardine Dussumiera acuta, anchovies Stolephorus sp., lanternsh Benthosema pterotum, and
various small jacks (family Carangidae) also contributing signicantly to the pelagic sh community in
certain areas.
In the rst cruise of the survey during May 1977, acoustic surveys indicated 91.6% of the region had a
low density of pelagic sh schools (8.72 schools/square nautical mile (NM2)), 7.6% had a medium density
of schools (24.53 schools/NM2), and 0.8% had a high density of schools (51.12 schools/NM2) (Junemann,
et al., 1981). The average density of the entire region was 11.63 schools/NM2. The estimated weight for
each school was 2.58 tons (t), giving an estimate of 26.43 t/NM2 or 613,023 t in the total study area. Most
of the schools resided in the upper 30 m of the water column, although several were recorded to a depth
of 85 m.
Three subsequent cruises between September 1977 and September 1978 indicated a noticeable annual
cycle in the biomass of small pelagic shes (Junemann, et al., 1981). Biomass estimates were higher in the
summer (1,720,000 t) and the fall (1,173,000 t) than in the early spring (252,000 t). These surveys also
detected a trend for increased biomass from north to south in the central Gulf and a lower biomass in the
Gulf of Oman. Throughout these cruises, the dominant taxa varied between the northwest and southeast
sections of the Gulf and also between the Iranian and Arabian side of the Gulf. Generally, S. sindensis, D.
acuta, and Stolephorus sp. were the major contributors to the small pelagic sh communities, although the
exact proportions of each species within each region varied by cruise. These cruises also reported dierent
diurnal behavioral patterns between sardines and anchovy and other shes. During the day, sardines and
anchovy form large schools, but they disperse more evenly through the water column when feeding at
night. Alternatively, carangids and myctophids, which formed a smaller proportion of the total pelagic sh
abundance, reside in deeper waters during the day and migrate to the surface at night.
Family Genus Species Common Name Presence in
Saudi Arabia
Scombridae Auxis thazard Frigate tuna Not recorded
Scombridae Euthynnus affinis Kawakawa Frequent
Scombridae Rastrelliger kanagurta Indian mackerel Frequent
Scombridae Sarda orientalis Striped bonito Rare
Scombridae Scomber australasicus Spotted chub mackerel Rare
Scombridae Scomber japonicus Chub mackerel Rare
Scombridae Scomberomorus commerson Narrow-barred Spanish mackerel Frequent
Scombridae Scomberomorus guttatus Indo-Pacific king mackerel Frequent
Scombridae Thunnus albacares Yellowfin tuna Frequent
Scombridae Thunnus tonggol Longtail tuna Rare
Istiophoridae Istiophorus platypterus Indo-Pacific sailfish Rare
Ariommatidae Ariomma indica Indian ariomma Frequent
Diodontidae Cyclichthys orbicularis Orbicular burrfish Frequent
Molidae Mola mola Ocean sunfish Rare
319
THE NATURAL ECOSYSTEMS OF THE WESTERN ARABIAN GULF
The dominant large pelagic species in the FAO survey included narrow-barred Spanish mackerel
Scomberomorus commerson, longtail tuna Thunnus tonggol, and kawakawa Euthynnus anus, with Indo-Pacic
king mackerel S. guttatus, frigate tuna Auxis thazard, queenshes Scomberoides sp., common dolphinsh
Coryphaena hippocampus, and barracudas Sphyraena sp. making up smaller portions of the community
(Junemann, et al., 1981). The most widely distributed of the large pelagic shes was S. commerson, which
was encountered throughout most of the study area. T. tonggol was present mostly in the Gulf of Oman,
although it was occasionally encountered in the southeastern Gulf. E. anis was mostly found in the
southeastern Gulf between September to December, spreading northwesterly during the warm season
from January until May.
From 2012 to 2015, the KFUPM Fisheries Program collected information about pelagic shes from
a review of literature, trawl surveys conducted from 2013 to 2015, landing site data collected in 2014, and
a pelagic acoustic survey conducted in 2015. The acoustic survey was conducted from April 20 to May 1,
2015, using three split-beam echosounders (Simrad EK60; Kongsberg Simrad AS, Kongsberg, Norway).
Twelve mid-water trawls were conducted to verify the species composition of sh schools detected by the
echosounders. Overall, the most abundant species were goldstriped sardinella Sardinella gibosa, buccaneer
anchovy Enchasicholina punctifer, and a non-identied species of anchovy, comprising 32%, 30% and 22% of
the total catch, respectively. The mean size of these species were 11.7 cm, 8.5 cm and 3.6 cm, respectively.
The results of the acoustic survey largely agreed with the FAO study (Junemann, et al., 1981) in that small-
sized sardines and anchovies contribute high biomass to the pelagic sh community and likely play and
important ecological role.
Fisheries on pelagic species by countries around the Gulf are dominated by artisanal shermen who
mostly target scombrids and carangids. Annual catches from 2010 for these two families were estimated to
be 45,000 t and 38,000 t, respectively (Al-Abdulrazzak, et al., 2013). According to the most recent FAO
data from 1997, these families were considered fully exploited in the Gulf. The majority of the catch of
pelagic shes was from Iran, Saudi Arabia, Qatar, and the UAE (Al-Abdulrazzak, et al., 2013). According
to Al-Abdulrazzak, et al. (2013), the amount of discarded bycatch of pelagic shes may be a signicant but
understudied issue in the Gulf.
Many pelagic shes are migratory, traveling long distances on a seasonal basis in search of prey or
to reach spawning areas. For some species, such as the Atlantic bluen tuna Thunnus thynnus and the
striped marlin Kajikia audax, migrations can cover thousands of kilometers and span entire ocean basins
(Squire, 1987; Block, et al., 2001). Dierential migration by separate segments of the population can
help identify stock structure, wherein distinct migratory units may occupy certain portions of a species’
range. Stock identication is a priority in sheries management to prevent overexploitation of vulnerable
migratory units (Begg and Waldman, 1999; Secor, 2004). Knowledge of migration patterns (e.g., distances
covered, seasonal movements, connectivity with other migratory units, etc.) is critical to ensure eective
management of pelagic shes. Such information is particularly important for stocks that cross international
boundaries where multinational cooperation is required to eectively manage the shared resource.
Several ecologically and economically important pelagic shes in the Gulf have broad species ranges
and are known to migrate long distances. Species such as S. commerson, S. guttatus, T. tonggol, E. anis,
cobia Rachycentron canadum, and Indo-Pacic sailsh Istiophorus platypterus are each distributed widely in
the Pacic Ocean or even globally (Serventy, 1956; Siddeek, 1995; Grandcourt, et al., 2005a). Migration
320
CHAPTER 3
patterns for several of these species have been identied within their total range, but their migrations
within and around the Arabian Gulf have been studied in detail for only Indo-Pacic sailsh (see Chapter
4.3 – Marine Fishes for discussion). Tagging studies for these species may provide important data on their
spatial and seasonal distributions, which could lead to improved management throughout the entire Gulf.
S. commerson is one of the most important pelagic sh species in the Gulf and is harvested mostly by
gillnet, longline, and handline. Grandcourt, et al. (2005) examined the S. commerson shery o the UAE
using age-based population dynamics. They found the shery was likely overexploited based on two
major ndings. First, the size at which sh were fully recruited to the shery was smaller than both the
mean size at maturity for females and the size for obtaining maximal yield per recruit. Second, the shing
mortality rate (F = 0.62/year) was larger than the precautionary target (F = 0.13/year) and limit (F =
0.17/year) biological reference points. Roa-Ureta (2015) applied generalized depletion models to the
S. commerson shery in Saudi Arabian waters. Based on the reconstructed history of the stock, he found
that the shing eort remained stable during the study period while the catch varied directly with the
magnitude of recruitment. Roa-Ureta (2015) concluded, contrary to the UAE shery, that shing pressure
on S. commerson is at sustainable levels, as indicated by an annual exploitation rate of 10%. Since S. commerson
in the Arabian Gulf, Gulf of Oman, and Arabian Sea are all part of the same genetic population (Hoolihan,
et al., 2006), these diering assessments could represent dierent stocks between the UAE and Saudi
waters. The assessment discrepancy highlights the need for a strategic regional approach to the assessment
and management of this, and other, highly migratory species.
Globally, over 7,500 structures related to oil and gas industries are found in coastal and pelagic waters of
53 countries (Parente, et al., 2006). These structures, comprised of pilings, pipes, and support beams, struts,
and cables, provide considerable vertical relief, eectively extending bottom complexity into the water
column and oering hard substrate where none was previously available. Oshore oil and gas platforms can
have positive eects on marine communities by providing settlement area for benthic organisms, protection
from predation, spawning habitat, and enhancing food production. These ecological benets have been
likened to those provided by articial reefs (Stanley and Wilson, 1997; Fabi, et al., 2004). Numerous studies
have shown that the biomass and abundance of marine organisms, including pelagic shes, is higher in the
immediate vicinity of oil and gas platforms (Fabi, et al., 2004; Niera, 2005; Scarcella, et al., 2011). Studies of
pelagic shes around oshore platforms often underestimate abundance and biomass near rigs due to the
diculty of collecting mobile shes within the connes of platform superstructures, meaning that the net
benet likely is higher than typically reported.
In the Saudi Arabian waters of the Gulf, hundreds of oil and gas platforms have been installed in
inshore and oshore areas. Rabaoui, et al. (2015) reported that the presence of oil and gas platforms within
a 5 km radius of sampling stations had a net positive eect on sh abundance, suggesting that the increase
in abundance was a result of the spillover eect. Biomass and biodiversity, however, were not aected by the
presence of nearby platforms. Current regulations in Saudi Arabia prevent access within a 500 m radius of
oil and gas platforms. Scarcella, et al. (2011) reported a linear decline in sh abundance with distance from
a platform in the Adriatic Sea with abundances several times higher within 50 m than at 250 m. Therefore,
it is likely that sh abundance closer to Saudi Arabian platforms is even higher than that reported by
Rabaoui, et al. (2015). The security perimeter maintained around Saudi oil and gas platforms eectively
creates a network of partial marine protected areas where shing eort is restricted. Pelagic shes common
321
THE NATURAL ECOSYSTEMS OF THE WESTERN ARABIAN GULF
in Saudi Arabian waters, such as herrings (Clupeidae), anchovy (Engraulidae), barracuda (Sphyraenidae),
jacks (Carangidae), and mackerels (Scombridae), have all been associated with pelagic oil and gas platforms
in other regions of the world (Franks, 2000). It is likely that these groups receive the most benet from the
network of oil and gas platforms in Saudi waters.
Trophic Structure
There are few data available for direct trophic interactions in the Gulf. Rather, the trophic structure
of the Gulf is assumed to follow a standard organization seen in oligotrophic waters worldwide (Calbet,
2008; Figure 3.110). The base of marine food webs globally is formed by phytoplankton, followed by
nanoagellates between 2 µm to 5 µm in size, (e.g., radiolarians and heterotrophic dinoagellates) and small
zooplankton (microzooplankton) between 5 µm and 200 µm in size. Microzooplankton includes tintinnids,
foraminifera, and small metazoans copepod nauplii and other small larvae. In the Arabian Sea, nanoagellates
dominate at low chlorophyll a concentrations, whereas the biomass of nanoagellates and microzooplankton
are similar during periods of high chlorophyll concentration (Garrison, et al., 2000). Calbet and Laundry
(2004) reported that these two groups can consume up to half of the available phytoplankton biomass per
day. It is likely that a similar trophic base exists in the Gulf. Primary consumers are grazed upon by larger
zooplankton (mesozooplankton), such as copepods and larval shes. The next trophic level are planktivorous
shes, such as small species of the families Clupeidae and Engraulidae, which feed on zooplankton. These
shes are abundant in the Gulf, due in part to the high primary production, which provides ample energy and
nutrients. Omnivorous and small piscivorous shes, such as the smaller species of carangids and scombrids,
rely on smaller shes and invertebrates as food sources. The highest trophic level is occupied by large shes,
such as marine mammals, sharks, and large species of scombrids and carangids.
Overall, more studies on the diet of key pelagic species are needed to develop an accurate model of the
Gulf pelagic food web. To date, diet studies have been limited to S. commerson (Grandcourt, et al., 2005a).
Many other species contribute to the pelagic marine food web in the Gulf, but their interactions will
remain unknown until further research is conducted.
Conclusions
The pelagic realm in the Gulf has been included in many ecological studies, but relatively few have
focused exclusively on pelagic habitats. More often, studies investigating coastal processes included stations
in pelagic waters. This means that the bulk of data related to the pelagic environment is scattered across the
literature. Consequently, there have been a few focused research programs on phytoplankton, zooplankton,
and shes in pelagic waters of the Gulf, which have provided valuable insights into the ecology of the
largest ecosystem in the Arabian Gulf.
Phytoplankton communities in the Gulf are dominated by a diverse diatom and dinoagellate assemblage,
with over 1,000 total species identied from the region. Species diversity and chlorophyll a concentrations
peak during cooler winter months, corresponding to high nutrient turnover. Subsequently, much of the
data on phytoplankton communities in pelagic waters of the Gulf comes from a single study, KFUPM/RI
322
CHAPTER 3
(2006c), which sampled 122 stations in pelagic waters o Saudi Arabia during 2002 and 2003. Additional
phytoplankton research throughout pelagic waters of the Gulf region, with an emphasis on documenting
species diversity and abundance, will likely reveal additional trends and patterns in other areas of the Gulf.
Zooplankton communities in the Gulf are dominated by copepods, which can account for over 80% of
total abundance. There is a general trend for higher abundance and diversity of zooplankton in the south,
Figure 3.110. Food web for pelagic waters of the Arabian Gulf.
323
THE NATURAL ECOSYSTEMS OF THE WESTERN ARABIAN GULF
near the Strait of Hormuz. Waters surrounding the Gulf are generally higher in diversity, which suggests
that physical and environmental conditions in the Gulf limit the zooplankton community. Likely, this is
related to the shallow depth of the Gulf compared to surrounding waters. As with phytoplankton studies,
few investigations have dealt explicitly with pelagic waters of the Gulf. Most information on zooplankton
in the pelagic realm comes from several studies that lacked methodological consistency. For example,
existing data are drawn from samples collected with nets ranging in mesh size from 100 µm to 333 µm and
using a mixture of oblique, vertical, and surface tows, making direct comparisons among studies dicult.
Finally, the taxonomic resolution of previous zooplankton studies varies greatly. Some identied broad
groups to the class level while others focused on specic groups and identied those to the genus level. No
studies have attempted species level identication of any pelagic zooplankton group.
Pelagic shes in the Gulf include some of the most ecologically and economically important species
in the entire Gulf region. Many species have been studied at the individual level, but there have been
relatively few broad-scale ecological studies of pelagic shes. An FAO survey used acoustic sonar, gillnet,
purse seine, and longline gear to look at pelagic shes o the UAE (Junemann, et al., 1981). Sardines were
the dominant small pelagic group, and S. commerson, T. tonggol and E. anus were identied as the most
abundant large pelagic taxa. Many of these species, particularly the large pelagic species, are migratory,
although the exact migratory routes and stock structure for these species is not clear. Such data are critical
for successful management of these shes, particularly since they are a shared resource among many Gulf
nations and may require regional cooperation to manage. Finally, oshore oil and gas platforms inuence
pelagic sh communities in many regions of the world. Given the abundance of articial structures in Gulf
waters, it is likely that pelagic shes derive some benet, although to what degree remains unclear.
While we have learned much about the patterns and trends of phytoplankton, zooplankton, and shes
in the pelagic realm of the Gulf in recent decades, focused eort on the pelagic ecosystem could tell us
much more about the ecology of pelagic waters. The biggest drawbacks of previous studies are that most
have included pelagic waters incidentally and have used a variety of sampling gears. These drawbacks
make assembling data on the pelagic realm dicult and limit the comparisons among studies. Considering
pelagic waters represent the largest ecosystem in the Gulf and are shared by eight of the nine nations
bordering the Gulf, an understanding of the dynamics of the pelagic ecosystem is essential to successful
management of one of the most important habitats in the region.
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571
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KFUPM/RI. 1999. Annual progress report: Sustaining research project —
Marine environmental studies. Fourth annual report. Prepared for
Saudi Aramco by the Water Resources and Environment Division,
Research Institute, King Fahd University of Petroleum and Minerals,
Dhahran, Saudi Arabia. Report Project No. 24154.
KFUPM/RI. 2000. Final report. Development of Red Sea biotope
maps using Remote sensing imagery. Prepared for Saudi Aramco
Environmental Protection Department by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Report Project
No. 24164.
KFUPM/RI. 2001. Final report: Sustaining research project — Marine
environmental studies. Phase III, Vol IV, Sustaining research
investigation Biological investigations: Coral reef monitoring,
primary productivity, mangrove transplantation. Prepared for Saudi
Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Report Project No. 24154.
KFUPM/RI. 2001a. Final report: Sustaining research project —
Marine environmental studies. Phase III, Vol I, Sustaining research
investigation — Monitoring of cooling water discharges [RT
Renery, Safaniyah GOSP-4] — Sediment Transport [Abu Ali Bay].
Prepared for Saudi Aramco by the Center for Environment and
Water, Research Institute, King Fahd University of Petroleum and
Minerals, Dhahran, Saudi Arabia. Report No. 24154.
KFUPM/RI. 2001b. Final report: Sustaining research project —
Marine environmental studies. Phase III, Vol II, Sustaining research
investigation — Environmental impact assessment of oshore
produced water. Prepared for Saudi Aramco by the Center for
Environment and Water, Research Institute, King Fahd University of
Petroleum and Minerals, Dhahran, Saudi Arabia. Report No. 24154.
KFUPM/RI. 2001c. Final report: Sustaining research project — Marine
environmental studies. Phase III, Vol. III, Sustaining research
investigation — Impacts of oshore drill cuttings disposal. Prepared
for Saudi Aramco by the Center for Environment and Water,
Research Institute, King Fahd University of Petroleum and Minerals,
Dhahran, Saudi Arabia. Report No. 24154.
594
REFERENCES
KFUPM/RI. 2001d. Final report: Sustaining research project — Marine
environmental studies. Phase III, Vol. IV, Sustaining research
investigation — Biological investigations: Coral reef monitoring,
primary productivity, mangrove transplantation. Prepared for Saudi
Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Report Project No. 24154.
KFUPM/RI. 2001e. Final report. Duba terminal permanent berth [BI-
8232] Prelimniary environmental assessment. Prepared for Lummus
Alireza Ltd. Co. by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Report Project No. CEW 2224.
KFUPM/RI. 2001f. Final report. Environmental impact assessment
for Abu Safah Oshore AM producing [300 MBCD] facilities
project [BI-3028]. Prepared for Saudi Aramco by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Report Project
No. CEW2236.
KFUPM/RI. 2002. Investigation of pollutant problems in Dammam
Corniche water. Prepared for the Directorate of Dammam by
Research Institute, King Fahd University of Petroleum and Minerals,
Dhahran, Saudi Arabia, Report Project.
KFUPM/RI. 2002a. Environmental impact assessment for the master
plan for marine works and coastal reclamation in the Al Khafji joint
operations concession area. Prepared for the Environmental Health
and Safety QTP Department, Al Khafji Joint Operations, Jiddah,
Saudi Arabia by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Report No. CEW2255.
KFUPM/RI. 2002b. Final report: Sustaining research project — Marine
environmental studies. Phase IV. Vol. 1-V. Prepared for Saudi Aramco
by the Center for Environment and Water, Research Institute, King
Fahd University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Report No. 24154.
KFUPM/RI. 2003a. Final report: Coral reef survey in support of the
marine and coastal damage assessment (OSDA). Prepared for the
Presidency for Meteorology and Environment, by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Report No.
CEW2257.
KFUPM/RI. 2003b. Final report: Oceanographic survey in support of
the marine and coastal damage assessment OSDA). Prepared for the
Presidency for Meteorology and Environment by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Report No.
CEW2256.
KFUPM/RI. 2004a. Final report: Oshore MP facilities Qatif 15 KV
Cable BI-8294) Environmental impact assessment. Prepared for the
Saudi Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Report No. CEW2278.
KFUPM/RI. 2004b. Duba Marine Terminal BI-8232) — Environmental
impact assessment for the construction and removal of temporary
roads. Prepared for the Saudi Aramco by the Center for Environment
and Water, Research Institute, King Fahd University of Petroleum
and Minerals, Dhahran, Saudi Arabia. Report No. CEW2259.
KFUPM/RI. 2005. Final report: Environmental impact assessment for
Manifa eld development (nafd/l-001-06): Causeway construction.
Prepared for the Arabian American Oil Company by the Center for
Environment and Water, Research Institute, King Fahd University of
Petroleum and Minerals, Dhahran, Saudi Arabia.
KFUPM/RI. 2005a. Environmental assessment of the breakwaters in
the Aziziyah area. Prepared for the Saad Trading and Contracting
Company, Al-Khobar, Saudi Arabia. Prepared by the Center for
Environment and Water, KFUPM/RI, July 2005. Project No.
CEW2304.
KFUPM/RI. 2005b. Final report: Environmental impact assessment
North Safaniyah articial lift [BI-10-00047]. Prepared for the
Saudi Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Report No. CEW2285.
KFUPM/RI. 2006. Environmental impact assessment for Manifa eld
development (Nafd/L-001-06): Causeway construction and
dredging. Prepared for Saudi Aramco, Dhahran, Saudi Arabia.
KFUPM/RI. 2006a. Final report: Environmental impact assessment
for Manifa eld development (NAFD/L-001-06): Causeway
construction and dredging. Prepared for Saudi Aramco by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Report No. CEW2328.
KFUPM/RI. 2006a. Section 2: Physical oceanography. pp. 25-97.
In: Oceanographic survey in support of the marine and coastal
damage assessment (Project Number CEW2256), Final report,
Vol. 1. Prepared for Presidency of Meteorology and Environment
(Dammam, Saudi Arabia) by the Center for Environment and
Water, King Fahd University of Petroleum and Minerals. Submitted
through Saudi Company for Environmental Works Ltd. (Al-Khobar,
Saudi Arabia), Dhahran.
KFUPM/RI. 2006a. Study of Al-Khafji seawater quality and marine
habitats (Project No. CEW2293). Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
KFUPM/RI. 2006b. Study of Al-Khafji seawater quality and marine
habitats. Prepared for Al-Khafji joint operations by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Report No.
CEW2293.
KFUPM/RI. 2006a. Study of Al-Khafji seawater quality and marine
habitats. Final report prepared for Al-Khafji joint operations by
the Center for Environment and Water, Research Institute, King
Fahd University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. CEW2293.
KFUPM/RI. 2006b. Environmental impact assessment for Manifa
eld development (NAFD/L-001-06): Causeway construction
recommended causeway conguration for engineering design
scoping (Project No. CEW2328). Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
KFUPM/RI. 2006b. Section 3: Chemical oceanography, pp. 98-180,
in: Oceanographic survey in support of the marine and coastal
damage assessment (Project Number CEW2256), Final report,
Vol. 1. Prepared for Presidency of Meteorology and Environment
(Dammam, Saudi Arabia) by the Center for Environment and
Water, King Fahd University of Petroleum and Minerals. Submitted
through Saudi Company for Environmental Works Ltd. (Al-Khobar,
Saudi Arabia), Dhahran.
KFUPM/RI. 2006c. Environmental risk and damage assessment of small
scale oil spill o the Al-Jubail coast, Arabian Gulf. Prepared for Saudi
Aramco Shell Renery Company SASREF) by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Report No.
CEW2301.
KFUPM/RI. 2006c. Section 5.3: Phytoplankton, pp. 280-343. In:
Oceanographic survey in support of the marine and coastal damage
assessment (Project No. CEW2256), Final report, Vol. 1. Prepared
for Presidency of Meteorology and Environment (Dammam, Saudi
Arabia) by the Center for Environment and Water, King Fahd
University of Petroleum and Minerals. Submitted through Saudi
Company for Environmental Works Ltd. (Al-Khobar, Saudi Arabia),
Dhahran.
KFUPM/RI. 2006d. Preliminary environmental assessment of marine
595
REFERENCES
ecology at the Qurayyah seawater treatment plant. Prepared for
the SNC-Lavalin Inc. by the Center for Environment and Water,
Research Institute, King Fahd University of Petroleum and Minerals,
Dhahran, Saudi Arabia. Report No. CEW2327.
KFUPM/RI. 2006e. Final report: Environmental baseline survey for
proposed central processing facilities at Khurais Prepared for
Saudi Company for Environmental Works Ltd. Al-Khobar by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Report No. CEW2321.
KFUPM/RI. 2006f. Final report: Duba marine terminal permanent berth
(BI-8232) Marine environmental impact assessment and monitoring
study. Prepared for Saudi Company for Environmental Works Ltd.
Al-Khobar by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Report No. CEW2259.
KFUPM/RI. 2006g. Environmental impact assessment of
decommissioning a portion of the breakwaters at Aziziyah, Arabian
Gulf. Prepared for Saad Trading and Contraction Company by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Report No. CEW2304.
KFUPM/RI. 2006h. Environmental impact assessment for the BerRI.
Causeway and associated drill site landlling. Prepared for Saudi
Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Project No. CEW2303.
KFUPM/RI 2006b. Environmental impact assessment for Manifa
Field development (NAFD/L-001-06): Causeway construction
recommended Causeway conguration for engineering design
scoping. Final report prepared for Saudi Aramco by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Project No.
CEW2328.
KFUPM/RI. 2007. Final report on “Oceanographic survey in support of
the marine and coastal damage assessment (II): Fisheries, ecosystem
analysis, databases and references.” Prepared for Presidency of
Meteorology and Environment, Dammam, Saudi Arabia. Report
Project No. CEW2256.
KFUPM/RI. 2007b. Environmental impact assessment for Manifa eld
development (NAFD/L): Causeway construction and dredging.
Prepared for Saudi Aramco by the Center for Environment and
Water, Research Institute, King Fahd University of Petroleum and
Minerals, Dhahran, Saudi Arabia. Project No. CEW2338.
KFUPM/RI. 2007c. Environmental impact assessment for Manifa
eld development: platforms, pipelines and submarine cables (BI-
10-00452 and BI-10-00453). Prepared for Saudi Aramco by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. CEW2338.
KFUPM/RI. 2007d. Environmental baseline survey: Manifa central
processing facilities (MCPF). Prepared for A. Al-Saihati, A. Fattani
and O. Al Othman Consulting Engineering Co., Al-Khobar, Saudi
Arabia by the Center for Environment and Water, Research Institute,
King Fahd University of Petroleum and Minerals, Dhahran, Saudi
Arabia. Project No. CEW2341.
KFUPM/RI. 2007e. Environmental impact assessment for Tanajib channel
and basin dredging. Prepared for Saudi Aramco by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Project No.
CEW2350.
KFUPM/RI. 2007. Sustaining research project, marine environmental
studies — Phase IV, Chapter II, Arabian Gulf coral reef monitoring.
Final report prepared for Saudi Aramco, by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Project No.
CEW2233.
KFUPM/RI. 2007f. Final report: Study of Al-Khafji seawater quality and
marine habitats. Prepared for Al-Khafji Joint Operations, Al-Khafji,
Saudi Arabia by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Report No. CEW2293.
KFUPM/RI. 2007a. Final report. Environmental impact assessment for
the New Arabia-Bahrain pipeline (BI-10-01110). Prepared for
the Arabian American Oil Company by Water and Environment
Division, Research Institute, King Fahd University of Petroleum and
Minerals, Dhahran, Saudi Arabia. Report Project No. CEW 2331.
KFUPM/RI. 2008. Final report: Sustaining research project — Marine
environmental studies. Phase IV, Vol. I, Sustaining research
investigation — Study of water quality and eutrophication in Saudi
Gulf coastal waters. Prepared for Saudi Aramco by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Report No.
CEW2233.
KFUPM/RI. 2008. The marine capture sheries of the Saudi Arabian
Gulf. White, S.T., Al-Suwailem, A.M. and Vivekanandan, E.V. (eds.).
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
KFUPM/RI. 2008. Environmental impact assessment for Karan platforms,
power (Bi-10-00579) and pipelines (Bi-10-00580) construction.
Final report submitted to Saudi Aramco, Dhahran, by Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Project Number
CEW 2357.
KFUPM/RI. 2008a. Environmental impact assessment for Karan
platforms, power (BI-1-00579) and pipelines (BI-10-00580).
Prepared for Saudi Aramco by the Center for Environment and
Water, Research Institute, King Fahd University of Petroleum and
Minerals, Dhahran, Saudi Arabia. Project No. CEW2357.
KFUPM/RI. 2008b. Final report. Saudi Aramco/KFUPM-RI sustaining
research project — Marine environmental studies — Phase IV —
Arabian Gulf coral reef monitoring. Prepared for Saudi Aramco by
the Center for Environment and Water, Research Institute, King
Fahd University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. 2233.
KFUPM/RI. 2009a. Environmental impact study for channel dredging at
Safaniyah. Prepared for Saudi Aramco by the Center for Environment
and Water, Research Institute, King Fahd University of Petroleum
and Minerals, Dhahran, Saudi Arabia. Project No. CEW2360.
KFUPM/RI. 2009b. Environmental impact assessment for the Ras Tanura
renery expansion project — Landlling and dredging. Prepared for
Saudi Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Project No. CEW2370.
KFUPM/RI. 2009c. Environmental impact assessment and monitoring
for drill cutting disposal at Manifa: Prepared for Saudi Aramco by
the Center for Environment and Water, Research Institute, King
Fahd University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. CEW2359.
KFUPM/RI. 2009a. Environmental impact assessment for the Ras Tanura
integrated project — Dredging. Prepared for Saudi Aramco by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. CEW2365.
KFUPM/RI. 2009f. Environmental impact assessment for the upgrade
of crude gathering and power supply facilities phase I — Safaniyah
eld. Prepared for Saudi Aramco by the Center for Environment
and Water, Research Institute, King Fahd University of Petroleum
and Minerals, Dhahran, Saudi Arabia. Project No. CEW2373.
KFUPM/RI. 2009e. Environmental impact study for the Ras Tanura
596
REFERENCES
integrated project — Dredging: Prepared for Kellogg Brown and
Root Saudi Limited Co. by the Center for Environment and Water,
Research Institute, King Fahd University of Petroleum and Minerals,
Dhahran, Saudi Arabia. Project No. CEW2361.
KFUPM/RI. 2009d. Development of operational marine modeling
system: Prepared for Saudi Aramco by the Center for Environment
and Water, Research Institute, King Fahd University of Petroleum
and Minerals, Dhahran, Saudi Arabia. Project No. CEW2325.
KFUPM/RI. 2009g. Environmental impact assessment for the Ras Tanura
renery expansion project — Landlling and dredging. Prepared for
Saudi Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Project No. CEW2370.
KFUPM/RI. 2009h. Marine environmental monitoring of the New
Khursaniyah 30” dia. pipeline (BI-10-08022) project. Prepared for
the Environment Protection Department, Saudi Aramco, by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. CEW2336.
KFUPM/RI. 2010a. Environmental impact assessment for the Ras Tanura
renery expansion project — Dredging and landlling. Prepared for
Saudi Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Final Report, Project No. CEW2370.
KFUPM/RI. 2010b. Marine environmental monitoring of the New
Khursaniyah 30” dia. pipeline (B1-10-08022) project. Prepared for
Saudi Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Final Report, Project No. CEW2336.
KFUPM/RI. 2010c. Marine environmental monitoring of the Manifa
causeway. Final report. Prepared for Saudi Aramco by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Project No.
CEW2342.
KFUPM/RI. 2010d. Environmental impact assessment for the upgrade
of crude gathering and power supply facilities phase 1 — Safaniyah
eld. Prepared for Saudi Aramco by the Center for Environment
and Water, Research Institute, King Fahd University of Petroleum
and Minerals, Dhahran, Saudi Arabia. Final Report, Project No.
CEW2373.
KFUPM/RI. 2010e. Environmental impact assessment for upgrade of
the re protection system, Ju’aymah oshore platform. Prepared for
Saudi Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Project No. CEW2381.
KFUPM/RI. 2010f. Environmental impact assessment for environmental
impact assessment for Arabiyah-Hasbah platforms, power (BI-10-
00916) and subsea pipelines (BI-10-00917). Prepared for Saudi
Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Project No. CEW2382.
KFUPM/RI. 2010e. Environmental impact assessment for installing
instrument scrapping facilities at Zuluf and Marjan oil elds.
Prepared for Saudi Aramco by the Center for Environment and
Water, Research Institute, King Fahd University of Petroleum and
Minerals, Dhahran, Saudi Arabia. Project No. CEW2379.
KFUPM/RI. 2010g. Environmental impact assessment for environmental
impact assessment for Arabiyah-Hasbah platforms, power (BI-10-
00916) and subsea pipelines (BI-10-00917). Prepared for Saudi
Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Project No. CEW2382.
KFUPM/RI. 2011. Environmental impact assessment for Arabiyah-
Hasbah platforms, power (BI-10-00916) and subsea pipelines (BI-
10-00917). Prepared for Saudi Aramco by the Water Resources and
Environment Division, Research Institute, King Fahd University
Petroleum and Minerals, Dhahran, Saudi Arabia. Report Project No.
CEW02382.
KFUPM/RI. 2012. Environmental assessment for the Tarut Bay pipelines
and structural support system. Prepared for Saudi Aramco by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. CEW2390.
KFUPM/RI. 2013. Final report. Saudi Aramco/KFUPM-RI sustaining
research project — Marine environmental studies — Phase V —
Arabian Gulf coral reef monitoring. Prepared for Saudi Aramco by
the Center for Environment and Water, Research Institute, King
Fahd University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. 2244.
KFUPM/RI. 2013b. Final report — Environmental impact assessment for
the expansion of two drill sites on the BerRI Causeway. Prepared for
Saudi Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Project No. CEW2400.
KFUPM/RI. 2013c. Final report — Environmental impact assessment
for dredging (category III) for upgrade of electrical power supply
to Abu Ali plants. Prepared for Zuhair Fayez Partnership by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. CEW2399.
KFUPM/RI. 2013e. Final report — Environmental impact assessment for
maintenance dredging to the existing Ras Tanura West pier basin and
channel. Prepared for Saudi Aramco by the Center for Environment
and Water, Research Institute, King Fahd University of Petroleum
and Minerals, Dhahran, Saudi Arabia. Project No. CEW2411.
KFUPM/RI. 2013f. First annual report — Monitoring and assessing
the marine environment in the vicinity of Saudi Aramco oshore
facilities in the Arabian Gulf. Prepared for Saudi Aramco by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. CEW2416.
KFUPM/RI. 2013g. Final report. Saudi Aramco/KFUPM-RI. sustaining
research project — Marine environmental studies — Phase V —
Arabian Gulf coral reef monitoring. Prepared for Saudi Aramco by
the Center for Environment and Water, Research Institute, King
Fahd University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. 2244.
KFUPM/RI. 2013a. Monitoring and assessing the marine environment
in the vicinity of Saudi Aramco oshore facilities in the Arabian
Gulf. Final report prepared for Saudi Aramco by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Project No.
CEW2416.
KFUPM/RI. 2013a. Final report — Oshore environmental baseline
survey in the Kingdom of Saudi Arabia sector for the Dorra oil eld
development. Prepared for WorleyParsons Europe Ltd. Middlesex,
United Kingdom by the Center for Environment and Water,
Research Institute, King Fahd University of Petroleum and Minerals,
Dhahran, Saudi Arabia. Project No. CEW2398.
KFUPM/RI. 2014a. Second annual report — Monitoring and assessing
the marine environment in the vicinity of Saudi Aramco oshore
facilities in the Arabian Gulf. Prepared for Saudi Aramco by the
Center for Environment and Water, Research Institute, King Fahd
University of Petroleum and Minerals, Dhahran, Saudi Arabia.
Project No. CEW2416.
KFUPM/RI. 2014b. Final report — Environmental impact assessment
for the new replacement Safaniyah Trunklines Tl-12 and Tl-13.
Prepared for Saudi Aramco by the Center for Environment and
Water, Research Institute, King Fahd University of Petroleum and
Minerals, Dhahran, Saudi Arabia. Project No. CEW2414.
597
REFERENCES
KFUPM/RI. 2014b. Status assessment and monitoring of the Saudi
Arabian waters of the Arabian Gulf. Final Report prepared for
Saudi Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Project No. CEW2416.
KFUPM/RI. 2014. Sustaining research project marine environmental
studies. Final report prepared for Saudi Aramco by the Center for
Environment and Water, Research Institute, King Fahd University
of Petroleum and Minerals, Dhahran, Saudi Arabia. Project No.
CEW2344.
KFUPM/RI. 2014. Aramco sustaining research project — environmental
studies. Fifth Final Report. Prepared for Saudi Aramco by Center for
Environment and Water, Research Institute, King Fahd University of
Petroleum and Minerals, Dhahran, Saudi Arabia. Unpublished.
KFUPM/RI. 2015. Sustaining research project: Marine environmental
studies, phase V. Final report submitted to the Arabian American Oil
Company by the Marine Studies Section, Center for Environment
and Water, Research Institute, King Fahd University of Petroleum
and Minerals, Dhahran, Saudi Arabia. Report Project No. 2344.
KFUPM/RI. 2015. Marine environmental monitoring of the Manifa
Causeway — Post-construction. Annual report prepared for Saudi
Aramco by the Center for Environment and Water, Research
Institute, King Fahd University of Petroleum and Minerals, Dhahran,
Saudi Arabia. Project No. CEW2410.
KFUPM/RI. 2015a. Final report: Sustaining research project —
Marine environmental studies. Phase V. Investigations on marine
environmental conditions in Saudi Arabian waters of the Arabian
Gulf. Prepared for Saudi Aramco by the Center for Environment
and Water, Research Institute, King Fahd University of Petroleum
and Minerals, Dhahran, Saudi Arabia. Report No. 2344.
KFUPM/RI. 2015b. Final Report. Environmental Impact Assessment
for the Hasbah oshore gas facilities increment II (BI-10-01902).
Prepared for Saudi Aramco by the Center for Environment and
Water, Research Institute, King Fahd University of Petroleum and
Minerals, Dhahran, Saudi Arabia. Project No. CEW2429.
KFUPM/RI. 2016. Fisheries program — Assessment and management
of essential sh habitats in Saudi Arabian waters. Draft nal report
under preparation for Saudi Aramco by the Center for Environment
and Water, Research Institute, King Fahd University of Petroleum
and Minerals, Dhahran, Saudi Arabia. Project No. CEW2375.
Khalaf, E., Literathy, P. and Anderlini, V. 1981. Vanadium as a tracer of
chronic oil pollution in the sediments of Kuwait. Proceedings of the
2nd International Symposium on Interaction between Sediment and
Freshwater, June 14-18, 1981, Kingston, Ontario, Canada.
Khaleghi Ghadiri, M. and Gorki, A. 2004. Natural remedies for impotence
in medieval Persia. International Journal of Impotence Research 16: 80-83.
Khan, M.A. and Al-Homaid, N.A. 2003. Remote sensing study on
mangrove depletion Tarut Bay, Saudi Arabia, pp. 227-233, in Alsharan,
A.S., Wood, W.W., Goudie, A.S., Fowler, A.R. and Abdellatif, E.M.
(eds.). Desertication in the 3rd Millenium. A.A. Balkema: Rotterdam.
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Reef corals and coral reefs of the Gulf of Oman is the first comprehensive photographic guide for the visual identification of scleractinian corals or true corals in the Sultanate of Oman. Illustrated with more than 850 color photographs, drawings and maps, it is designed to help divers as well as scientists to distinguish the many species of corals encountered along the gulf of Oman. More than 120 species have been catalogued and photographed in the coastal communities of the Sultanate.