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A sufficient knowledge on prehistoric culture and habitat of earliest Homo sapiens (Balangoda man) is available in Batadomba-lena cave, a noticeable rock shelter in lowland rainforest of southwestern Sri Lanka goes upto Pleistocene and Holocene eras. Late Pleistocene inhabitants of Batadombalena cave's foraged for a broad spectrum of plant and mainly arboreal animal resources such as, monkeys, squirrels and rainforest snails etc. Archaeo-faunal evidence would help to describe the prehistoric man eating behavior as well as availability of nature prehistoric flora, fauna and environmental status. The family Acavidae is very sensitive to climatic variations, hence used as a bio-indicator to describe the variations of paleo-climatic nature. This study examined the morphological features of 20 samples of Acavidae family (living/fossil samples of Acavus superbus, and sub fossil samples of Oligospira waltoni) collected from soils by digger method in 2005 and compared with 20 samples from the same area at presently available. The shell characters of snails such as, height, width, diameter of mouth, thickness of lip, and angular of axis were measured and subjected to multivariate analysis to understand how climatic variability and nature of paleo-diet contribute survival of Acavidae species. Results showed that Acavus superbus living species had large shell characteristics than the sub fossils. Results of similar study in the same climatic status in 2000 showed that the shell measurements of Acavus superbus are relatively larger than both living and sub fossils in Batadobalena cave. Ordination diagram derived from species shell characteristics showed that Acavus superbus living species grouped as scattered /diffuse clusters, while sub fossil species grouped as a single cluster at the center of the ordination diagram. It is imply a trend of speciation /diversification of Acavus species from Pleistocene era to date. Multivariate analyses prove that, a strong positive correlation of species characteristics, such as height (r = 0.62), thickness of lip (r = 0.544) and angular of axis (r = 0.744), and a strong negative relationship (r = 0.832) for shell width for the species were observed. Our results are useful to compare with other fossil snails to see whether the climate change influence for changing body size. In conclusion, palaeo-environment, and present environment variation has been occurred in minimum way without much changes to observed Acavidae species compositions present and past.
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Annals of Valahia University of Targoviste. Geographical Series (2016), 16(2): 59-68
DOI: 10.1515/avutgs-2016-0005
ISSN (Print): 2393-1485, ISSN (Online): 2393-1493
MORPHOLOGICAL VARIATION AND SPECIATION OF ACAVIDAE
FAMILY: A CASE STUDY FROM FOSSIL AND LIVING SPECIES OF
BATADOMBALENA CAVE PRE-HISTORIC SITE IN SRI LANKA
Aravinda Ravibhanu Sumanarathna1, Buddhika Madurapperuma2, Janaka
Kuruppuarachchi3, Jinadasa Katupotha4, S.M.K.Abeywardhana5, Pathmakumara
Jayasinghe6
1,3Faculty of Natural Sciences, The Open University of Sri Lanka, Email: Ara22ravibhanu@gmail.com
1The Faculty of Natural and Environmental Sciences, University of Southampton, United Kingdom
2Department of Forestry and Wildland Resources, Humboldt State University, Arcata, CA, USA
1,5,6South Asian Astrobiology & Paleobiology Research Unit of Eco Astronomy Sri Lanka
6National Building Research Organization, Jawatta Rd., Colombo, Sri Lanka
1,5Postgraduate Institute of Archaeology, University of Kelaniya, Sri Lanka
4Department of Geography, University of Sri Jayewardenepura, Sri Lanka
Abstract
A sufficient knowledge on prehistoric culture and habitat of earliest Homo sapiens
(Balangoda man) is available in Batadomba-lena cave, a noticeable rock shelter in lowland rainforest of
southwestern Sri Lanka goes upto Pleistocene and Holocene eras. Late Pleistocene inhabitants of
Batadombalena cave’s foraged for a broad spectrum of plant and mainly arboreal animal resources such as,
monkeys, squirrels and rainforest snails etc. Archaeo-faunal evidence would help to describe the prehistoric
man eating behavior as well as availability of nature pre-historic flora, fauna and environmental status. The
family Acavidae is very sensitive to climatic variations, hence used as a bio-indicator to describe the variations
of paleo-climatic nature. This study examined the morphological features of 20 samples of Acavidae family
(living/fossil samples of Acavus superbus, and sub fossil samples of Oligospira waltoni) collected from soils by
digger method in 2005 and compared with 20 samples from the same area at presently available. The shell
characters of snails such as, height, width, diameter of mouth, thickness of lip, and angular of axis were
measured and subjected to multivariate analysis to understand how climatic variability and nature of paleo-diet
contribute survival of Acavidae species. Results showed that Acavus superbus living species had large shell
characteristics than the sub fossils. Results of similar study in the same climatic status in 2000 showed that
the shell measurements of Acavus superbus are relatively larger than both living and sub fossils in
Batadobalena cave. Ordination diagram derived from species shell characteristics showed that Acavus
superbus living species grouped as scattered /diffuse clusters, while sub fossil species grouped as a single
cluster at the center of the ordination diagram. It is imply a trend of speciation /diversification of Acavus
species from Pleistocene era to date. Multivariate analyses prove that, a strong positive correlation of species
characteristics, such as height (r = 0.62), thickness of lip (r = 0.544) and angular of axis (r = 0.744), and a
strong negative relationship (r = 0.832) for shell width for the species were observed. Our results are useful to
compare with other fossil snails to see whether the climate change influence for changing body size. In
conclusion, palaeo-environment, and present environment variation has been occurred in minimum way
without much changes to observed Acavidae species compositions present and past.
Keywords: Acavidae, Paleoecology, Batadombalena Cave, Sabaragamuwa Basin, Sri Lanka
1. INTRODUCTION
Paleoecology uses geological and biological evidences from fossil deposits to investigate the
past occurrence, distribution, and abundance of different ecological units on a variety of time scales,
which provides scientific evidence for present and future. The Sabaragamuwa Basin, Sri Lanka
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provides dominant type of natural Palaeo-eco-evidences (Deraniyagala 1958). The cultural remains
of early man of this area were discovered together with the skeletal fragments and geometric
microliths. Other detections include various types of fauna and flora that are thought to have formed
part of human diet, also the animal bones, which was fossilized adjoining the Sabaragamuwa Basin
called “Rathnapura Fauna” (Fig. 1). As a result of the palaeo-diet of Balangoda man (Homo
sapiens),who lived in cave of pre historic site, Batadombalena cave (38,000 BP) which was the
proper harbor life station( Aravinda et al 2016), accumulated many snails (Acavidae species), such
as Acavus phoenix, Acavus superbus, and Oligospira waltonias fossil deposits.
Figure 1. Historic overview of Batadobalena cave in Sabaragamuwa Basin. A: Paronomic view (west to
east) of the Sabaragamuwa Basin, B: Batadobalena cave Pre Historic Site, C: Batadobalena cave rock shelter and
excavation trench, D: Biththipodi Ella (BDA1) and D1-D3 represent the Faunal Diversity of BDA1 , E:Paranomic
view of Sabaragamuwa Basin (During the Pleistocene epoch, Sri Lanka has experienced heavy rainfall and the entire
island was covered with rain forests. These heavy showers created large lakes and marshes in Sabaragamuwa Basin
providing habitats for a number of marsh loving mammals and other animals). F: A synthesis representation of the
Balangoda man, G: Pre historic artifacts and microlithic
The Batadombalena cave measures approximately 15 m high, 18 m wide, and 25 m in
length, totaling the internal cave area to 6,800 m2. It is located at 5 km away from the town of
Kuruwita, Sabaragamuwa Province of Sri Lanka (Fig. 2).
There were fragmented human remains and stone artifacts were discovered by Deraniyagala
(1938) at Batadombalena cave by his excavation. This study site was excavated up to four feet and
assigned the assemblage of stone artifacts, in particular the association of microliths and human
remains, related to the Balangoda phase. Then, a preliminary examination was made in 1979 was
explored rich occupational deposit in the site. Thereafter, the strait graphic sequence of seven main
occupational layers and three underlying strata directly above the bedrock has been described by
Daraniyagala in 1982 by an excavation of 2.6 meters. Layers 1 3 from top downwards were
considered to have been described in resent time. The occupational deposited in layer 4 was
described as a massive homogenous stratum with brownish sand and silt containing stone artifacts
and faunal remains. Layers 5 and 6 were very important and considered to be the site’s major
occupational layer. In addition, layer 7 contains many stone artifacts including geometric microliths
which were radiocarbon dated to Ca. 30 000 years BP.
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Figure 2. A detail map of Batadombalena Cave located at the Kuruwita in Sabaragamuwa
province in Sri Lanka
Acavidae is a taxonomic family of air-breathing land snails, terrestrial pulmonate gastropod
mollusks in the super family Acavoidea (Bouchet and Rocroi 2005). Acavidea has been surviving
and adapting to the terrestrial life in wet zone from the pre-historic time. Sub fossils of Acavidae
have recorded as a dominant place from the optimal fossils, which were found in every excavation
in Batadombalena cave. Occupation of Acavoidea species in different soil strata proved that the
Acavidae members were been lived continually throughout each paleo-era Batadombalena area.
There are number of different Acavidae species of snails are most abundant dispersal surrounding,
76 acres of Batadombalena cave forest area at present. The objective of this study is to compare
morphological characteristics of shell of existing species of Acavidae family live in surrounding
areas at Batadombalena cave with that of fossils of Acavidae members.
2. METHODS
Family Acavidaeis very sensitive to climatic variations and therefore, it can be used as a bio-
indicator to describe the variations of paleo-climatic nature and present. This study examined the
morphological features of 20 samples of Acavidae family collected from soils by digger method in
2005. The shell characters of Acavidae such as, shell height, width, diameter of mouth, thickness of
lip, and angular of axis were measured. Then, fossil record data were compared with 20 samples
from the same area at presently available (Fig. 3). The shell characters in each individual were used
to create a data matrix for multivariate analyzing. The ordination methods of Detrended
Correspondence Analysis (DCA) were tested using PC-ORD 4 software to select the best
correlation between ordination axes and shell characters.
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Figure 3. Family Acavidae samples from Batadombalena cave (A block: Living samples of Acavus
superbus: A1,A2,A3, A4; B block: samples from 2005 excavation of Acavus
superbus,B1,B2,B3,B4; and C1: Oligospira waltoni
3 RESULTS AND DISCUSSION
Sri Lanka has a variety of forest types which provide habitats for different snail species. The
wet south-western region and the central highlands are covered with tropical rain forests, sub-
montane forests and wet evergreen forests particularly at higher elevations. Tropical semi-evergreen
forests are present in the transition zone between the wet zone and the dry zone. The lowland wet
zone forests, the study site Batadombalena cave belongs, occupy only less than 20% of the
landmass of the country with more than 55% of human population. The major part of the dry zone
has tropical dry mixed evergreen forests. There are number of studies carried out to recognize the
effect of global climatic changes on natural forests of Sri Lanka. Kuruppuarachchi et al. (2016)
recognized that dry zone forests are more vulnerable for future global climatic changes. Similarly, it
has been predicted that there would be a northward shift of tropical wet forest into areas currently
occupied by tropical dry forest (Somaratne and Danapala 1996). Thus, it is clear that more
interactions with climatic parameters would arise in the tropical forests in the future climatic change
scenarios. Thus, due to drastic changes of climatic conditions may seriously affect to the
composition or abundance of snail living in Batadombalena cave, wet lowland tropical area of Sri
Lanka. The comparison analyzing between palaeo-environment and present environment of
Batadombalena cave was reproduced by variation of species composition of snails at said eras. We
compare shell characters of Acavus superbus for living species (A1- A4) and sub fossils (B1 B4)
and the results are shown in Fig. 3 and Table 1.The results showed that, the Acavidae species,
which was lived early period can be identify in the same zone at present.
Measurements: Acavus superbus living species: (n=20); Diameter of mouth (D): 26.7-39.3
mm, x
̅ = 32.3± 5.4 mm; Height (H): 31.2 -36.8 mm, x
̅ = 33.3 ± 2.4 mm; D/H: 0.85-1.07 mm, x
̅ =
0.97 ± 0.10 mm.
Acavus superbus sub fossils: (n=20); D: 30.6-34.4 mm, x
̅ = 32.1 ± 1.6 mm; H: 30.3-33.2
mm, x
̅ = 32.1 ± 1.3 mm; D/H: 0.95-1.05 mm, x
̅ = 1.0 ± 0.10 mm.
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0
10
20
30
40
50
60
B1 B2 B3 B4 C1 A1 A2 A3 A4
mMeasurement (mm)
Species Reference Number
Height Width Diameter Thickness
Table 1. Comparison characters of living Acavidae species with relevant fossil Acavidaea samples
of Batadombalena cave (Living species = 1#,Sub fossils =1, Non-foramen of shell = 2#,
Foramen of shell =2)
A1 Acavus superbus 1# 32.2 41.12 33.27 10.75 52° 2#
A2 Acavus superbus 1# 36.76 50.47 39.26 5.898 52° 2#
A3 Acavus superbus 1# 33.22 42.93 30.01 5.624 54° 2#
A4 Acavus superbus 1# 31.18 44.34 26.70 4.231 52° 2#
B1 Acavus superbus 1 33.04 54.36 34.44 5.865 53° 2
B2 Acavus superbus 1 30.32 47.86 31.96 5.817 50° 2
B3 Acavus superbus 1 31.71 52.30 30.63 7.278 52° 2
B4 Acavus superbus 1 33.2 48.33 31.56 7.038 53° 2
C1
Oligospira waltoni
1 22.63 53.01 26.51 5.333 40° 2#
Thickness
of lip (mm)
Special
features
Reference
Number
Fossil species
Living species/
sub fossils
Height
(mm)
Width
(mm)
Diameter of
mouth (mm)
According to the above measurements, Acavus superbus living species had large shell
characteristics than the sub fossils. In addition, we compared our species shell characteristics of the
same species with research finding of Hausdore and Perera (2000) at Rakwana which is belong to
the same eco-climatic region. The results showed that the shell measurements of Acavus superbus
in Rakwana (D: 33.6-52.5 mm, x
̅ = 47.2± 3.7 mm; H: 33.9-47.8 mm, x
̅ = 42.7 ± 2.9 mm; D/H:
0.88-1.35 mm, x
̅ = 1.11 ± 0.108 mm) was relatively larger than both living and sub fossils in
Batadobalena cave. Therefore, it can be concluded that, palaeo-environment, and present
environment variation has been occurred in minimum way without much changes to the snail
compositions present and past. If snails are comparatively environmental sensitive, changes of
environmental parameters of study area for last Ca. 30,000 years period were not been considerable
affect for change of morphology of shell or snail species.
We compared the shell characteristics, such as height, width, diameter and thickness of
living Acavidae species with relevant fossil Acavidae samples (Fig. 4). The fossil Acavidae samples
showed a less variability among individuals of shell characteristics except width. In contrast, living
Acavidae species showed a distinct variability of individual shells except thickness.
Figure 4. Comparison characteristic chart of living Acavidae species with relevant fossil
Acavidae samples of Batadombalena cave
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Due comparison characteristic of living Acvidae species with relevant fossil acavidae
samples of Batadombalena cave, there are minimum variations between limitation factors of pre
historic and present condition of Sabaragamuwa Basin. According to calculation of structured of
snails shell, direction of the heat flow of depend on angular of axis (Fig. 5). Comparison calculation
in between angular of axis, height, thickness of lip, diameter of mouth and width of living with
fossil Acavidae samples are dominantly delineating approximately conformation.
The relationship of Acvidae species and its shell characters were compared using ordination
axes 1 and 2 by overlaying species main matrix with each characteristics (Figs. 6a, 6b, 6c, 6d, and
6e). In the ordination diagram, Acavus superbus living species (A1- A4) grouped as separate
/diffuse clusters, while A. superbus sub fossil species grouped as a single cluster at the center of the
ordination diagram. Figures 6a to 6d showed that a speciation /diversification trend of Acavus
species from Pleistocene era to date. This signifies that the living species have more structural
variability than fossil species. On the other hand, Oligospira waltoni separated along Aix 1
remarkably than those A. superbus living/sub fossil species. There are strong positive correlation of
species characteristics, such as height (r = 0.62), thickness of lip (r = 0.544) and angular of axis (r =
0.744). In contrast, shell width showed a strong negative relationship (r = 0.832) among species.
Figure 5. The temperature distribution and heat flow in and around a snail exposed to sun on the
dry and wet surface. Direction of the heat flow indicated by broken arrows
There are still many more unidentified variables can be influenced for speciation and
distribution of modern-day animal and plant communities. Studies on this field are provide
constantly improving understanding of interactions among and between communities and species
due to climatic variability are important for recognizing future trends and sustainable conservation
of sensitive species such as Acavidae. Niche theory has attempted to salve these questions some
extent regarding living communities. The development of concepts, such as niche width and
overlap, specialization and inter and intra-specific competition would be described the said
problems. Increases in the mean body size of the individuals, fluctuations in availability of food
supply and in rainfall, competition (intra or inter-specific), predation and the environment in which
the animals live are all suggested as factors would be affected for the mammal populations. These
concepts have provided explanations for the behavior observed within many animal communities
with competition appearing to be a significant driving force behind species diversity and density.
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Figure 6a. Ordination living/ sub-fossil Acavidae species overlaid by height to show their
correlation along ordination axes.
Figure 6b. Ordination living/ sub-fossil Acavidae species overlaid by width to show their
correlation along ordination axes.
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Figure 6c.Ordination living/sub-fossil Acavidae species overlaid by diameter of mouth to show
their correlation along ordination axes.
Figure 6d. Ordination living/ sub-fossil Acavidae species overlaid by thickness of lip to show their
correlation along ordination axes.
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Figure 6e. Ordination living/ sub-fossil Acavidae species overlaid by angular of axis to show their
correlation along ordination axes.
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... The number of identified fragments from layer 7 is much greater than from layers 4 to 6, along the lines of excavations from 2005 [2]. Family Acavidae is very sensitive to climatic variations and therefore, it can be used as a bio indicator to describe the fluctuations of Palaeo-climatic nature and present day [10], [65]. Therefore, Acavus identifications, continuously found in seven layers, with wide vertical spreads, which led us there , would certainly be no grounds to suspect environmental change in the environs of Batadomba-Lena [2], [10]. ...
... From the optimal fossils found in every excavation in Batadombalena cave, sub fossils of Acavidae have been reported as a dominant position [64]. Occupation of Acavidae species in different soil strata showed that the members of the Acavidae were ceaselessly lived in each Batadombalena region of the Palaeo age [64], [65]. ...
... If there was a dry or arid season in the wet zone, the prehistoric man would have little chance of getting wet zone animals here. But when we consider the population of all the seven layers of Batadombalena, it does not appear that there is a decrease in the population [2], [62]- [65]. ...
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The fossils are preserved remains of body parts or traces of ancient organisms. Sri Lanka is a continental island that evolved via unique geological formations, including fossil remains. This island represents many fossils belonging to three different geological periods, for instance: the Jurassic period, Miocene period, and Pleistocene epoch. Most of the Pleistocene fossils were found in terrestrial deposits (alluvial) from the Sabaragamuwa basin called Ratnapura fauna. Thus, our investigations focused on documenting samples of fossils gathered, under the project called "The Paleo World of Sabaragamuwa Basin-Sri Lanka" conducted by Eco Astronomy Inc (Sri Lanka). Considering the geological time scale, we are looking for reporting samples that approximately belong to the Quaternary period. As we know, the Quaternary period of the Earth's geographic history includes two geologic epochs viz., which are: the Pleistocene (2.58 Myr to 0.0012 Myr), and the Holocene (0.0012 Myr to Present). Both epochs have changed and divided the fauna's equilibrium and human's cultural phases based on climate and sea-level fluctuations that took place during these periods. Some of the sections in those epochs has occurred during the last glacial maximum (LGM) and represent the mean sea level was much lower compared with the present records. Therefore, the quaternary period shows the open accessibility to migration of mammalian mega faunal species, that lived during the transition from the Pleistocene to the Holocene epoch. Most probably, the terrestrial climate change has impacted them and caused the extinction of those megafaunas. The gathered data details were synchronized via the technical aspect of sampling photography, toy photography, and virtual reality for analyses and reconstruction purposes.
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Geotourism is 'tourism that focuses on geology and landscape as the basis for providing visitor engagement, learning, and enjoyment'. Geotourism and geo-heritage are relatively new form of tourism with considerable Sri Lanka and global growth potentials. Interest in geotourism is developing at a very rapid rate around the world. It is of great importance to support and enhance the global movement about geotourism generally and specifically into geo land mark included geo-heritage sites. The country like Sri Lanka represents an area rich with numerous geological and geomorphological formations which are excellent representatives of this area's geodiversity since Archean eon to present. However, the geotourism potential of these geo sites still remains fully unrevealed and neglected. For many millennia, the prehistoric community has been concerned about the unrestricted appreciation of sites of geological or geomorphic interest. The features of geologic or geomorphic interests, based on folds, faults and topographic relief provide spectacular vistas and unique opportunities to learn about earth's geologic processes and history. This should be our geological heritage, which represents the collective memory of the Mother Nature. Geotourism is essentially 'geological tourism'. The geological element focuses on geology and landscape and includes both 'form', such as landforms, rock outcrops, rock types, sediments, soils and crystals, and 'process', such as volcanism, erosion, glaciation etc. The tourism element of geotourism includes tourists visiting, learning from, appreciating and engaging in geo sites. Thus, the nature of the abiotic geological heritage involves a sustainable, viable and responsible tourism development that enhances the wellbeing of the local communities.
Technical Report
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Danigala Circular Rock [ Lat: 7°40'50.24"N | Lon : 81°12'48.32"E ] is a unique geological rock situated in near Kandegama in the Polonnaruwa district. The aerial view of the rock show a unique semi-circular shape, affected by geological activities and weathering conditions. The location of Danigala represents an area rich with numerous geological and geomorphological formations, which are excellent representatives of this area's geodiversity abundance since the Precambrian era to present. The distinction of environmental elements relevant to archeology, astronomy, biodiversity, and cultural factors makes this land unique. In 28th July 2020, we have documented a new discovery of Petroglyphs that have been found in a part of the northwest slope direction of Danigala inselberg. Those bind runes are dominantly compared with other archeological sites in Sri Lanka and South Asia region. The type of symbols(bind runes) and petroglyphs found are quite new and for the first time discovered in Sri Lanka during archaeoastronomical and geological preliminary survey conducted by The Central Cultural Fund (CCF- Polonnaruwa-Alahana Parivena Project) with the corporation of South Asian Astrobiology & Earth Sciences Research unit of Eco Astronomy Sri Lanka. Hence, this is new discovery should be considered as our geological, astronomical, and archeological heritage site, which represents the collective memory of the anthropomorphic scenes, affected by Mother nature. Thus, those facts we propose that this exotic area get involved in a sustainable management, a viable and responsible tourism development base on Geo tourism, Astro tourism, Archeo tourism and Adventure tourism via a multidisciplinary approach that enhances the well being of the local communities.
Presentation
The knowledge of Martian geology has increased enormously in the last 40 yr. Several missions orbiting or roving Mars have revolutionized our understanding of its evolution and geological features, which in several ways are similar to Earth, but are extremely different in many respects. The impressive dichotomy between the two Martian hemispheres is most likely linked to its impact cratering history, rather than internal dynamics such as on Earth. Mars’ volcanism has been extensive, very longlived and rather constant in its setting. Water was available in large quantities in the distant past of Mars, when a magnetic field and more vigorous tectonics were active. Exogenic forces have been shaping Martian landscapes and have led to a plethora of landscapes shaped by wind, water and ice. Mars’ dynamical behavior continues, with its climatic variation affecting climate and geology until very recent times.
Presentation
The knowledge of Martian geology has increased enormously in the last 40 yr. Several missions orbiting or roving Mars have revolutionized our understanding of its evolution and geological features, which in several ways are similar to Earth, but are extremely different in many respects. The impressive dichotomy between the two Martian hemispheres is most likely linked to its impact cratering history, rather than internal dynamics such as on Earth. Mars’ volcanism has been extensive, very longlived and rather constant in its setting. Water was available in large quantities in the distant past of Mars, when a magnetic field and more vigorous tectonics were active. Exogenic forces have been shaping Martian landscapes and have led to a plethora of landscapes shaped by wind, water and ice. Mars’ dynamical behavior continues, with its climatic variation affecting climate and geology until very recent times.
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This study investigated the relationships amongst floristic, soil and climatic parameters and their control on carbon sequestration (CS) in two selected forest stands of Sri Lanka. Representative sam-pling sites were selected from the dry zone (Sigiriya forest sanctuary) and the wet zone (Udawattakele forest reserve) of Sri Lanka. Litter and soil samples were collected from each sampling site randomly in monthly intervals to cover an annual cycle. Plant biomass carbon stocks were calculated using standard biomass equations. Soil carbon stocks were determined by chemical oxidation and loss on ignition (LOI) methods. Principle Factor Analysis and multiple regression were used to quantify the relationships among the plants, soil and climatic variables. Plant biomass carbon stocks of the forests were governed by labile and stable C fractions, soil moisture, and plant diversity. The soil fulvic fraction acts as a focal point of interacting the variables such as soil N, free litter fraction (FLF) and humic fraction. During dry period in the dry zone forest, CS was governed by maximum relative humidity through an atmosphere-floor litter-soil continuum. Air temperature and FLF play a vital role in determining soil N. In addition, MacIntosh distance (U) diversity index showed a significant positive relationship with soil N. The dry zone forests are seen to be more climatic sensitive and vulnerable than the wet zone forests in Sri Lanka due to influence of more climatic parameters that govern the soil organic carbon fractions.
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The genus Acavus from Sri Lanka includes three species, Acavus haemastoma (Linnaeus), Acavus superbus (L. Pfeiffer) and Acavus phoenix (L. Pfeiffer) with two subspecies, Acavus phoenix phoenix (L. Pfeiffer) and Acavus phoenix castaneus new subspecies. The conchological and anatomical differences between these species, as well as their intraspecific variation are described. Their distribution is shown on maps and all locality records are listed. The presence of extensive intraspecific polymorphism, the development of geographical subspecies and the presumable hybridization between some species show that the Acavus species are not isolated relict species, but that speciation is in progress and that the radiation of the Acat lu species is probably much younger than the radiation of the acavid genera. The three Acavus species are not acutely endangered at present. In contrast to many other land snails, there is no risk of a rapid decline of the Acavus species due to deforestation, because these species also occur in synanthropic habitats.
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A second extinct big cat, tentatively considered to be a tiger (Panthera tigris), is recorded from Sri Lanka for the first time from a fossil left lower carnassial found in alluvium near Ratnapura in 1962 and a sub-fossil right middle phalanx 14 C dated to ~ 16,500 ybp, discovered in 1982 in a prehistoric midden at Batadomba Cave, near Kuruwita. The species is diagnosed from the only other big cats known from Sri Lanka, Panthera pardus and the extinct P. leo sinhaleyus Deraniyagala, 1938. This record significantly advances the timing of dispersal of tigers into the Indian peninsula. Tigers appear to have arrived in Sri Lanka during a pluvial period during which sea levels were depressed, evidently prior to the last glacial maximum ca. 20,000 years ago. The lion appears to have become extinct in Sri Lanka prior to the arrival of culturally modern humans, ca. 37,000 ybp.
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According to solar nebula structured ,our planetary system bear from accretion of the dust particles and planetesimal period, after that condensation in solar nebula. Thus most of celestial bodies of our planetary system,like planet,natural satellite,comet, meteorite & asteroids exhibit the different kind of planetary habitable. Base on energy source as a sun like star, carbon as a most prominent element of life forms on earth & percentage of liquid water which consist of celestial bodies. Due to study of the origin,evolution, distribution & future of life in universe , earth is the only place know to harbor life. It is depend on minimal condition for life such as temperature,water,radiation shielding,the stuff of life , sunlight, oxygen, when planet belongs to G2 type star forming like ours. To revealed evidences for the planetary habitability & harbor life of planet earth, paleontological factors are the one of most prominent way . It’s provide a unique view into the history of life by showing the forms and features of life in the past & tell us how species have changed across long periods of the Earth’s history. Though the fossil record does not include every planet and animal that ever lived, also compatibility substantial evidence for the common descent of life via evolution & tend to explain about other habitable planets(one upon which living beings not unlike terrestrial organisms) like Gliese 581c & Kepler-452b which consisted in out of our solar system. There are massive possibility of habitable zone around other stars & search for extraterrestrial microbial life,such as found from the examination of the Allan hills 84001 meteorite like microfossil .Also undeniable fossils (meteorite type) which carried out from aranaganwila _sri lanka , exhibited the ample evidences for extraterrestrial microbial life. Thus our aims to be explore dominate paleontological factors (Macro fossils/ Pleistocene) in sabaragamu basin sri lanka,which tend to explain comparative model of Harbor life of planet earth.
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Using a combination of biostratinomic and early diagenetic phenomena, it is possible to recognize a series of taphonomic facies (or taphofacies) within sedimentary sequences. Interpretation of taphofacies elucidates many aspects of ancient sedimentary environments which are otherwise unrecognizable. Finally, comparative taphonomy provides an unequivocal means for recognition of rapid, episodic deposition. Detailed taphonomic analysis of shallow-marine rocks proves that many sequences are comprised largely of episodic deposits. In turn, certain well-characterized event beds with unique taphonomic histories may provide easily mapped and isochronous markers for local correlation and basin analysis.-from Authors
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A comparison of species richness of leaf litter samples derived from a variety of modern forest types provides a means for estimating diversity of source forests in the fossil record. The major differences in methods needed for reconstruction of source forest richness from forests in different climatic zones indicates that a climatic filter should be applied to estimates of plant diversity in the past. -from Author
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Modern biodiversity hotspots are characterized by high species diversity and by biotas facing a substantial threat of extinction, largely due to a high proportion of endemic taxa living in these regions. Theoretically, hotspots of biodiversity are areas of particular interest in the fossil record because of the relatively high quality and quantity of data that they may contribute to a global understanding of vegetational response to changes in climate, tectonic uplift, and ecological disturbance. Current models for climatic reconstruction that depend on leaf physiognomy are based on data sets in which species-rich tropical floras are less well represented, relative to temperate floras. Eight modern Neotropical floras from a range of precipitation regimes were evaluated to determine the influence that high source floral diversity has on reconstruction of mean annual temperature (MAT) and mean annual precipitation (MAP). Floras are drawn from sites in Costa Rica to southern Peru, having species richness from 55 to >400 species per plot. MAT of the sites spans a range of 24 to 28°C, and MAP ranges from ∼1600 mm to 3000 mm. By subsampling the modern floras in rank order of dominance (basal area), the importance of collecting intensity and completeness on subsequent assessments of MAT and MAP is evaluated. Biodiverse floras are good at reconstructing MAT if at least 50% of the species are included. When only 25 species are used for temperature calculations, the accuracy of the parameter is compromised, but a ±3°C error encompasses the majority of the deviation. Application to the early Paleocene Castle Rock fossil flora of Colorado confirms the validity of subsampling in high-diversity fossil applications. However, reconstruction of MAP is fraught with problems that do not appear to be related to biodiversity of the floras. Errors on estimates of MAP currently are so large as to make the values too vague to be useful in most applications. This study has accepted a 20% error as necessary, but the applicability of data with errors > 20% is questionable in situations where rainfall is >1500 mm per year. MAP estimates using leaf area are almost universally underestimates of actual MAP, and frequently are >400 mm in error. Exploration of these data indicates that effort would be well placed in investigating the relative importance of precipitation parameters in altering leaf morphology before choosing one to reconstruct climates of the past.
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The potential impact of climate change on forest distribution in Sri Lanka was evaluated. The Holdridge Life Zone Classification was used along with current climate and climate change scenarios derived from two general circulation models, the Geophysical Fluid Dynamics Laboratory model and the Canadian Climate Centre Model, at a 0.5 0.5 resolution. Current and future distributions of life zones were mapped with a Geographic Information System. These maps were then used to calculate the extent of the impact areas for the climate change scenarios. The current distribution pattern of forest vegetation includes tropical very dry forest (6%), tropical dry forest (56%), and tropical wet forest (38%). Results obtained using the Geophysical Fluid Dynamics Laboratory model show an increase in tropical dry forest (8%) and decrease in tropical wet forest (2%). The Canadian Climate Centre Model scenario predicted an increase in tropical very dry forest (5%) and tropical dry forest (7%), and a decrease in tropical wet forest (11 %). Both models predicted a northward shift of tropical wet forest into areas currently occupied by tropical dry forest. The application of general circulation models such as the Geophysical Fluid Dynamics Laboratory model and the Canadian Climate Centre Model, as well as the Holdridge Life Zone Classification, to estimate the effect of climate change on Sri Lankan forests in this paper indicates that these methods are suitable as a tool for such investigations in Sri Lanka.