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  • 1
    Online Resource
    Online Resource
    London :Taylor & Francis Group,
    Keywords: Marine biodiversity. ; Electronic books.
    Description / Table of Contents: Biodiversity loss in terrestrial environments associated with human activities has been appreciated as a major issue for some years now. What is less well documented is the effect of such activities, including climate change, on marine biodiversity. This pioneering book is the first to address this important but neglected topic, which is likely to be the key challenge for marine scientists in the near future. Using a multidisciplinary and a holistic approach, the book reveals how climatic variability controls biodiversity at time scales ranging from synoptic meteorological events to millions of years and at spatial scales ranging from local sites to the whole ocean. It shows how global change, including anthropogenic climate change, ocean acidification and more direct human influences such as exploitation, pollution and eutrophication may alter biodiversity, ecosystem functioning and regulating and provisioning services. The author proposes a theory termed the 'macroecological theory on the arrangement of life', which explains how biodiversity is organized and how it responds to climatic variability and anthropogenic climate change. The book concludes with recommendations for further research and theoretical development to identify oceanic areas in need of observation and gaps in current scientific knowledge. Many references and comparisons with the terrestrial realm are included in all chapters to better understand the universality of the relationships between biodiversity, climate and the environment. The book will serve as a textbook for all students and researchers of marine science and environmental change, but will also be accessible to the more general reader.
    Type of Medium: Online Resource
    Pages: 1 online resource (519 pages)
    Edition: 1st ed.
    ISBN: 9781136462863
    Series Statement: Earthscan Oceans Series
    DDC: 577.6
    Language: English
    Note: Cover -- Title -- Copyright -- Dedication -- Contents -- Acknowledgements -- 1 Introduction -- 1.1 Biodiversity from the land to the ocean -- 1.2 Classification and census of marine biodiversity -- 1.3 Organisation of the book -- PART I Natural environmental variability and marine biodiversity -- 2 Large-scale hydro-climatic variability -- 2.1 The composition and structure of the atmosphere -- 2.2 The earth radiation budget -- 2.3 The thermal engine -- 2.4 Main climatic regions -- 2.5 The oceanic hydrosphere -- 2.6 Hydro-climatic variability -- 3 Large-scale biogeographic patterns -- 3.1 Biogeography: from the terrestrial to the marine realm -- 3.2 Primary compartments of the marine ecosphere -- 3.3 Ecogeographic patterns -- 4 Large-scale biodiversity patterns -- 4.1 The search for a primary cause -- 4.2 Neutral and null models or theories -- 4.3 The area hypothesis -- 4.4 History -- 4.5 Hypotheses based on fundamental processes -- 4.6 The climatic influence -- 4.7 Temperature -- 4.8 Environmental hypotheses -- 4.9 Evolutionary rate -- 4.10 Biotic interactions -- 5 Marine biodiversity through time -- 5.1 Palaeoclimatic changes -- 5.2 Natural causes of extinction -- 5.3 Natural contemporaneous changes -- 5.4 Is climate the primary factor? -- 6 Temperature and marine biodiversity -- 6.1 Temperature from the origin of the universe to early life -- 6.2 Basics and first principles -- 6.3 Effects of temperature at the physiological level -- 6.4 Influence of temperature at the species level -- 6.5 Thermal influence at the community level -- PART 2 Marine biodiversity changes in the Anthropocene -- 7 Biodiversity and anthropogenic climate change -- 7.1 Human alteration of the greenhouse effect and the radiative budget of the planet -- 7.2 Increase in global air and sea surface temperature -- 7.3 Species responses to anthropogenic climate change. , 7.4 Community/ecosystem response to climate change -- 7.5 Anthropogenic climate change and natural hydro-climatic variability -- 8 Marine biodiversity and ocean acidification -- 8.1 Introduction -- 8.2 Anthropogenic acidification -- 8.3 Effects of acidification on biodiversity -- 8.4 Limitations of past studies on ocean acidification -- 8.5 Conclusions -- 9 Biodiversity and direct anthropogenic effects -- 9.1 Exploitation of marine biodiversity -- 9.2 Pollution -- 9.3 Nutrient enrichment and eutrophication -- 9.4 Oxygen depletion -- 9.5 Introduction and invasion of exotic species -- 9.6 UV-B radiation -- 9.7 Tourism -- 9.8 Extinction -- 9.9 Interactive effects -- 10 Marine biodiversity, ecosystem functioning, services and human well-being -- 10.1 Biodiversity and ecosystem functioning -- 10.2 Biodiversity changes and ecosystem goods and services -- 10.3 Potential effects of changes in marine biodiversity for global biogeochemistry -- 10.4 Potential feedbacks -- PART 3 Theorising and scenarising biodiversity -- 11 Theorising and scenarising biodiversity -- 11.1 Introduction -- 11.2 The concept of the ecological niche -- 11.3 Rationale of the METAL theory -- 11.4 The METAL theory -- 11.5 Strength and assumptions of the METAL theory -- 11.6 Limits to predictions in the context of global change -- 11.7 Scenarising biodiversity -- 12 Conclusions -- 12.1 A macroscopic approach -- 12.2 Global monitoring -- 12.3 Towards a unifying ecological theory -- References -- Index -- Colour Plates.
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  • 2
    Type of Medium: Book
    Pages: 75 S , graph. Darst., Kt
    Series Statement: Marine ecology progress series 2004, Suppl.
    Language: English
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Global change biology 9 (2003), S. 0 
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: Recently, large-scale changes in the biogeography of calanoid copepod crustaceans have been detected in the northeastern North Atlantic Ocean and adjacent seas. Strong biogeographical shifts in all copepod assemblages were found with a northward extension of more than ° in latitude of warm-water species associated with a decrease in the number of colder-water species. These changes were attributed to regional increase in sea surface temperature. Here, we have extended these studies to examine long-term changes in phytoplankton, zooplankton and salmon in relation to hydro-meteorological forcing in the northeast Atlantic Ocean and adjacent seas. We found highly significant relationships between (1) long-term changes in all three trophic levels, (2) sea surface temperature in the northeastern Atlantic, (3) Northern Hemisphere temperature and (4) the North Atlantic Oscillation. The similarities detected between plankton, salmon, temperature and hydro-climatic parameters are also seen in their cyclical variability and in a stepwise shift that started after a pronounced increase in Northern Hemisphere Temperature anomalies at the end of the 1970s. All biological variables show a pronounced change which started after circa 1982 for euphausiids (decline), 1984 for the total abundance of small copepods (increase), 1986 for phytoplankton biomass (increase) and Calanus finmarchicus (decrease) and 1988 for salmon (decrease). This cascade of biological events led to an exceptional period, which is identified after 1986 to present and followed another shift in large-scale hydro-climatic variables and sea surface temperature. This regional temperature increase therefore appears to be an important parameter that is at present governing the dynamic equilibrium of northeast Atlantic pelagic ecosystems with possible consequences for biogeochemical processes and fisheries.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 426 (2003), S. 661-664 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The Atlantic cod (Gadus morhua L.) has been overexploited in the North Sea since the late 1960s and great concern has been expressed about the decline in cod biomass and recruitment. Here we show that, in addition to the effects of overfishing, fluctuations in plankton have resulted in ...
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2023-01-13
    Keywords: Author(s); Database accession number; Reference/source; Title; Uniform resource locator/link to reference; Year of publication
    Type: Dataset
    Format: text/tab-separated-values, 837 data points
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  • 6
    Publication Date: 2024-02-16
    Description: The database collected using the Continuous Plankton Recorder (CPR) operated by SAHFOS covers a long time span (surveys are on-going since 1946) and the whole North Atlantic, including the North Sea. It is therefore a unique tool to investigate changes in the planktonic community composition. Key publications have documented, for example, changes in zooplankton and chlorophyll abundance over the past decades. However, the data on calcareous plankton archived in the CPR database have not yet been exploited. The publication of the "Atlas of Calcifying Plankton" by SAHFOS and EPOCA begins to fill this gap and is therefore most timely. I am convinced that the scientific community will use this short preliminary description of the data available to investigate the drivers of the changes (or lack of thereof) reported in the Atlas.
    Keywords: Bivalvia sp., larvae; Clione limacina; Coccolithophoridae sp.; Date/time end; Date/time start; Echinodermata, larvae; EPOCA; European Project on Ocean Acidification; Foraminifera, planktic; LATITUDE; Limacina retroversa; LONGITUDE; Microscopy
    Type: Dataset
    Format: text/tab-separated-values, 36176 data points
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  • 7
    Publication Date: 2018-12-17
    Description: Aim Following the biogeographical approach implemented by Longhurst for the epipelagic layer, we propose here to identify a biogeochemical 3-D partition for the mesopelagic layer. The resulting partition characterizes the main deep environmental biotopes and their vertical boundaries on a global scale, which can be used as a geographical and ecological framework for conservation biology, ecosystem-based management and for the design of oceanographic investigations. Location The global ocean. Methods Based on the most comprehensive environmental climatology available to date, which is both spatially and vertically resolved (seven environmental parameters), we applied a combination of clustering algorithms (c-means, k-means, partition around medoids and agglomerative with Ward's linkage) associated with a nonparametric environmental model to identify the vertical and spatial delineation of the mesopelagic layer. Results First, we show via numerical interpretation that the vertical division of the pelagic zone varies and, hence, is not constant throughout the global ocean. Indeed, a latitudinal gradient is found between the epipelagic–mesopelagic and mesopelagic–bathypelagic vertical limits. Second, the mesopelagic layer is shown here to be composed of 13 distinguishable Biogeochemical Provinces. Each province shows a distinct range of environmental conditions and characteristic 3-D distributions. Main conclusions The historical definition of the mesopelagic zone is here revisited to define a 3-D geographical framework and characterize all the deep environmental biotopes of the deep global ocean. According to the numerical interpretation of mesopelagic boundaries, we reveal that the vertical division of the zone is not constant over the global ocean (200–1,000 m) but varies between ocean basin and with latitude. We also provide evidence of biogeochemical division of the mesopelagic zone that is spatially structured in a similar way than the epipelagic in the shallow waters but varies in the deep owing to a change of the environmental driving factors.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2018-10-11
    Type: Article , NonPeerReviewed
    Format: text
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  • 9
    Publication Date: 2024-02-07
    Description: Planktonic Foraminifera are unique paleo-environmental indicators through their excellent fossil record in ocean sediments. Their distribution and diversity are affected by different environmental factors including anthropogenically forced ocean and climate change. Until now, historical changes in their distribution have not been fully assessed at the global scale. Here we present the FORCIS (Foraminifera Response to Climatic Stress) database on foraminiferal species diversity and distribution in the global ocean from 1910 until 2018 including published and unpublished data. The FORCIS database includes data collected using plankton tows, continuous plankton recorder, sediment traps and plankton pump, and contains similar to 22,000, similar to 157,000, similar to 9,000, similar to 400 subsamples, respectively (one single plankton aliquot collected within a depth range, time interval, size fraction range, at a single location) from each category. Our database provides a perspective of the distribution patterns of planktonic Foraminifera in the global ocean on large spatial (regional to basin scale, and at the vertical scale), and temporal (seasonal to interdecadal) scales over the past century.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2017-02-02
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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