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Estado de conservación de la Flora de la Región Mediterránea: realidad y retos de futuro

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Abstract

La cuenca del Mediterráneo alberga una de las floras más ricas y diversas del mundo, formada por unas 25.000 especies (Greuter, 1991 y 1994; Médail & Quézel, 1997), gran parte de la cual, más del 50 % según algunas estimaciones, es endémica de este territorio o de alguno de los que los países ribereños. Sin embargo, su estudio y conocimiento está aún lejos de ser completo. Simplemente el inventario, la relación de especies que viven en este territorio, no ha podido completarse pese a los esfuerzos realizados en las últimas décadas del siglo XX y las primeras del XXI (Greuter et al., 1984-2008). Sirvan como ejemplo las aún inacabadas floras de Grecia (Strid & Tan, 1997-2002) o la Península Ibérica (Castroviejo, 1986-2019), los dos extremos del Mediterráneo, donde se concentra la mayor diversidad de especies (Heywood, 2002; Aedo et al., 2013).

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This publication has been prepared by IUCN (International Union for Conservation of Nature). The designation of geographical entities in this book, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of the European Commission or IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of the European Commission or IUCN
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A detailed study of 15 sediment cores from Blanes Canyon and its immediate surroundings (NW Mediterranean Sea) was conducted to compare historic sedimentation rates and evaluate the possible impact of bottom-trawling intensification on the sedimentary regimes over the past 50 years. The canyon axis and flanks, as well as the adjacent open slope, were sampled at water depths ranging from 300 m to 2200 m. Grain size, dry bulk density, and ²¹⁰Pb concentration profiles were measured to assess possible changes in sedimentation rates over the last century and their temporal and spatial relationship to bottom trawling effort. Sedimentation rates in the upper canyon axis (900–1200 m) had the highest rates of 0.9–2.1 cm·yr⁻¹, quantified since the 1970s. Farther downcanyon, sedimentation rates increased two to five times after the 1970s, from 0.1–0.2 cm·yr⁻¹ to 0.2–0.8 cm·yr⁻¹, which coincides with a rapid growth of the total engine power of the fishing fleet operating in the study area. The enhanced sedimentation rates occur downslope of the main fishing grounds and decrease downcanyon as the distance from trawling grounds increases. These results highlight the ability of bottom trawling to resuspend bottom sediments, leading to net erosion of the canyon rims and flanks. In turn, large volumes of sediment are advected towards the canyon's interior, ultimately increasing sediment deposition along the canyon axis. Natural sedimentation rates at similar along-canyon distance from shore in the untrawled continental slope (900–1500 m) and in the lower canyon axis (1500–2200 m) are comparable (0.08–0.20 cm·yr⁻¹), suggesting distance from coastal sediment sources as the main control on regional sedimentation in deeper parts of the margin. While submarine canyons have been regarded as preferential cross-margin conduits for sediment dispersal, they can also potentially function as modern depocenters for trawling-induced sedimentation.
Article
The Global Strategy for Plant Conservation (GSPC) seeks to assess the conservation status of the world vascular plants by 2020, and to guarantee that at least 75% threatened taxa are conserved in situ. A comprehensive evaluation of IUCN categories for 7269 Spanish vascular plants (GSPC Target 2), using distribution data and environmental niche models, is presented. A gap analysis to assess the percentage of threatened plants effectively conserved in situ (considering national parks, plant micro-reserves and recovery or conservation plans) was also conducted (Target 7). The result is that only 44.4% threatened species are subject to an adequate in situ protection. An appropriate management of additional natural protected areas towards the conservation of threatened plants would make Spain meet this threshold, but severe deficiencies should be corrected. The methodology presented here is proposed as a tool to assess the degree of achievement of GSPC targets. This procedure can be quickly implemented and allows an easy evaluation of the progress, as well as the pending tasks in a given period of time.
Article
In the Mediterranean, blue whiting, Micromesistius poutassou, constitutes a traditional fisheries resource. Over several decades, blue whiting landings in the Catalan coast (northwestern Mediterranean) have displayed cyclical variations, of c. 6 yrs, slightly decreased to five in the last two decades, as shown through wavelet analysis. These fluctuations have persisted under very different levels of fishing effort. This study evaluates the hypothesis that deep-water formation in the adjacent Gulf of Lions, and the enhanced primary productivity related to it, determines recruitment strength in blue whiting that results ultimately in the observed periodicity of the blue whiting landings. The link between landings and environmental drivers was explored using lagged cross-correlations, with 0- and 1-yr lag. The variables considered included large-scale indices [North Atlantic Oscillation (NAO) and the Atlantic Multi-decadal Oscillation (AMO)], Mediterranean climate indices [MO and Western Mediterranean Oscillation (WeMO)], and variables defining the local environmental conditions in the northwestern Mediterranean (sea-air heat flux, winter air temperature anomaly and Rhône river runoff). Significant correlations were only found between landings (1961-2011) and sea-air heat flux, which is generally taken as an indicator of processes of deep water convection, at 0 and 1-yr lag. These results suggest that the observed fluctuations in blue whiting landings respond to oceanographic processes taking place in the Gulf of Lions.
Article
Outlines the early evolution of the Tethys and Mediterranean seas, including comments on the evolution of the Atlantic Ocean and the relationships of the alpine belts to the genesis of the Mediterranean basin. Closer attention is paid to the evolution of the W Mediterranean Basin, examining the Balearic Basin, Alboran Sea and Tyrrhenian Sea, and noting the stratigraphic record of this region. Global events leading to the Messinian salinity crisis when, during the Late Miocene, the Mediterranean became separated from the Atlantic, and geological evidence for this crisis are reviewed, and a dynamic model of the crisis is essayed. Regional depositional patterns during the Pliocene and Quaternary are discussed, particularly in terms of likely primary factors influencing sedimentation, and an attempt is made at modelling these phenomena.-P.J.Jarvis
Article
This paper reports the re-discovery of Barbarea auriculata Hausskn. ex Bornm. var. auriculata (Brassicaceae), Onobrychis nitida Boiss. (Fabaceae), Onosma discedens Hausskn. ex Bornm. (Boraginaceae), and Silene oligotricha Hub.-Mor. (Caryophyllaceae). All of these taxa had been listed as Extinct (EX), according to the World Conservation Union Red List Categories. This study provides the re-descriptions of these taxa, presents field observations of these taxa, and suggests new IUCN categories.
Article
The overall counterclockwise alongslope circulation of Atlantic Water (AW) in the western basin of the Mediterranean Sea is now generally accepted. As the eastern basin displays similar general features, why is it generally assumed to function in a different way, and why is AW now said to circulate across the interior of the eastern basin? Relatively huge mesoscale anticyclonic eddies induced by the instability of the AW circulation in the south of the western basin have lifetimes up to several years. It is possible that they extend down to the sea bottom and play a major role in the distribution of all water masses. Why have apparently similar eddies generated in the eastern basin never received specific attention? Once formed, Mediterranean Waters (MWs) must spread and circulate before outflowing. Why have simple dynamical arguments for understanding the circulation of AW, such as the Coriolis effect, rarely been considered for the circulation of MWs? In this paper we address these major aspects of water circulation in the Mediterranean Sea. In order to be as objective and convincing as possible, and to write a paper that can be understood by as broad a readership as possible, we have chosen to present only raw data sets that can be easily interpreted by the reader without any help from the author. Based on the evidence provided by these data sets, we specify the current debates and list what we think are the main unanswered questions.
Article
The Valencian region, in eastern Spain, is home to ≈3050 vascular plant species, 68 of which are listed under the critically endangered IUCN category. To afford protection to our endangered, rare and endemic flora, a network of small (2–20 ha) statutory reserves has been created by the Regional Wildlife Service. These are termed “micro-reserves” and encompass a large number of individual species and natural habitats. The objective is to monitor long term changes in the plant populations and to carry out active management of the protected plants. In the selection of plots, criteria of distinctiveness and endangerment of plants was followed. Eight years after the onset of this initiative, plant micro-reserves have become an essential tool for the effective protection of the diverse flora of this Mediterranean region.
Article
Aim: Predicting the impact of climate change on marine ecosystems or how fish and other species are adapting to rising sea temperatures is still subject to much uncertainty, despite considerable progress in recent years. In this study we assess whether our understanding of the impact of sea warming on marine fish can be enhanced with an interdisciplinary approach that collates data from fisheries, fishermen and scientific research. By doing this, we aim to shed light on the major changes in the abundance and diversity of warm and cold water fish in recent decades in relation to sea warming. Location: This study was conducted in the north-western Mediterranean, where the impacts of global warming are particularly critical because range shifts are physically constrained. Methods: We collected and combined statistical data from fisheries, the traditional ecological knowledge of fishermen (TEK), reproductive data (histological gonad analyses and ichthyoplankton surveys) and extensive research into the relevant literature (including systematic catalogues and museum collections and their databases). Results: We have found that changes in the abundance of fish have followed a particular spatio-temporal sequence, with three different phases of colonization in the case of warm-water species (occasional occurrence, common presence and establishment), and three phases of regression (abundance reduction, range contraction and disappearance from the catch) in the case of cold-water species. Main conclusions: Overall, the results show that this multidisciplinary approach, combining qualitative and quantitative information from different sources, provides new insight into the observed changes in fish diversity and abundance in relation to climate change.