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  • 1
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Ecology -- Antarctica. ; Biotic communities -- Antarctica. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (586 pages)
    Edition: 1st ed.
    ISBN: 9781444347210
    DDC: 577.0998/9
    Language: English
    Note: ANTARCTIC ECOSYSTEMS: An Extreme Environment in a Changing World -- CONTENTS -- Contributors -- INTRODUCTION: ANTARCTIC ECOLOGY IN A CHANGING WORLD -- Introduction -- Climate change -- The historical context -- The importance of scale -- Fisheries and conservation -- Concluding remarks -- References -- PART 1: TERRESTRIAL AND FRESHWATER HABITATS -- 1 SPATIAL AND TEMPORAL VARIABILITY IN TERRESTRIAL ANTARCTIC BIODIVERSITY -- 1.1 Introduction -- 1.2 Variation across space -- 1.2.1 Individual and population levels -- 1.2.2 Species level -- 1.2.3 Assemblage and ecosystem levels -- 1.3 Variation through time -- 1.3.1 Individual level -- 1.3.2 Population level -- 1.3.3 Species level -- 1.3.4 Assemblage and ecosystem levels -- 1.4 Conclusions and implications -- Acknowledgments -- References -- 2 GLOBAL CHANGE IN A LOW DIVERSITY TERRESTRIAL ECOSYSTEM: THE MCMURDO DRY VALLEYS -- 2.1 Introduction -- 2.2 The McMurdo dry valley region -- 2.3 Above-belowground interactions -- 2.4 The functioning of low diversity systems -- 2.5 Effects of global changes on coupled above-belowground subsystems -- 2.6 Temperature change: warming -- 2.7 Temperature change: cooling -- 2.8 Direct human influence: trampling -- 2.9 UV Radiation -- 2.10 Concluding remarks -- Acknowledgements -- References -- 3 ANTARCTIC LAKES AS MODELS FOR THE STUDY OF MICROBIAL BIODIVERSITY, BIOGEOGRAPHY AND EVOLUTION -- 3.1 The variety of antarctic lake types -- 3.2 The physical and chemical lake environment -- 3.3 The microbial diversity of antarctic lakes -- 3.3.1 Methods for exploring Antarctic lake biodiversity -- 3.3.2 Microbial groups -- 3.3.3 Protists -- 3.3.4 Crustacea -- 3.4 Biogeography -- 3.4.1 Spatial variation and the global ubiquity hypothesis -- 3.4.2 Temporal variation and palaeolimnology -- 3.5 Evolution -- 3.5.1 Prokaryote physiology -- 3.5.2 Eukaryote physiology. , 3.6 Future perspectives -- 3.7 Acknowledgement -- References -- PART 2: MARINE HABITATS AND REGIONS -- 4 THE IMPACT OF REGIONAL CLIMATE CHANGE ON THE MARINE ECOSYSTEM OF THE WESTERN ANTARCTIC PENINSULA -- 4.1 Introduction -- 4.1.1 The oceanographic setting -- 4.1.2 The historical context -- 4.2 Predicted environmental changes along the western antarctic peninsula -- 4.3 Environmental variability and ecological response -- 4.3.1 Biotic responses to climate change: some general points -- 4.4 Responses of individual marine species to climate change -- 4.4.1 Acclimation and evolutionary responses to environmental change in antarctic marine organisms -- 4.5 Community level responses to climate change -- 4.6 Ecosystem level responses to climate change -- 4.7 What biological changes have been observed to date? -- 4.8 Concluding remarks -- Acknowledgements -- References -- 5 THE MARINE SYSTEM OF THE WESTERN ANTARCTIC PENINSULA -- 5.1 Introduction -- 5.2 Climate and ice -- 5.2.1 Surface air temperature -- 5.2.2 Sea ice -- 5.2.3 Climate co-variability -- 5.3 Physical oceanography -- 5.4 Nutrients and carbon -- 5.4.1 Nutrients and UCDW intrusions -- 5.4.2 Carbon cycle -- 5.4.3 Dissolved organic carbon -- 5.4.4 Sedimentation and export -- 5.5 Phytoplankton dynamics -- 5.5.1 Seasonal scale dynamics -- 5.5.2 Role of light -- 5.5.3 Role of nutrients -- 5.5.4 Annual variability in phytoplankton -- 5.6 Microbial ecology -- 5.7 Zooplankton -- 5.7.1 Community composition and distribution -- 5.7.2 Long-term trends and climate connections -- 5.7.3 Grazing and biogeochemical cycling -- 5.8 Penguins -- 5.8.1 Contaminants in penguins -- 5.9 Marine mammals -- 5.10 Synthesis: food webs of the wap -- 5.11 Conclusions -- Acknowledgements -- References -- 6 SPATIAL AND TEMPORAL OPERATION OF THE SCOTIA SEA ECOSYSTEM -- 6.1 Introduction -- 6.2 Oceanography and sea ice. , 6.2.1 Upper-ocean circulation and characteristics in the Scotia Sea -- 6.2.2 Physical variability and long-term change -- 6.3 Nutrient and plankton dynamics -- 6.4 Krill in the scotia sea food web -- 6.4.1 Krill distribution in the Scotia Sea -- 6.4.2 Krill growth and age in the Scotia Sea -- 6.4.3 Krill reproduction and recruitment in the Scotia Sea -- 6.4.4 Krill - habitat interactions in the Scotia Sea -- 6.4.5 Krill population variability and change in the Scotia Sea -- 6.4.6 Krill in the Scotia Sea food web -- 6.5 Food web operation -- 6.5.1 Trophic links -- 6.5.2 Spatial operation of the food web -- 6.6 Ecosystem variability and long-term change -- 6.7 Concluding comments -- Summary -- Acknowledgements -- References -- 7 THE ROSS SEA CONTINENTAL SHELF: REGIONAL BIOGEOCHEMICAL CYCLES, TROPHIC INTERACTIONS, AND POTENTIAL FUTURE CHANGES -- 7.1 Introduction -- 7.2 Physical setting -- 7.3 Biological setting -- 7.3.1 Lower trophic levels -- 7.3.2 Mid-trophic levels -- 7.3.3 Fishes and mobile predators -- 7.3.4 Upper trophic levels -- 7.3.5 Benthos -- 7.4 Food web and biotic interactions -- 7.5 Conclusions -- 7.5.1 Uniqueness of the Ross Sea -- 7.5.2 Potential impacts of climate change -- 7.5.3 Conservation and the role of commercial fishing activity in the Ross Sea -- 7.5.4 Research needs and future directions -- Acknowledgements -- References -- 8 PELAGIC ECOSYSTEMS IN THE WATERS OFF EAST ANTARCTICA (30 E-150 E) -- 8.1 Introduction -- 8.2 The region -- 8.2.1 The east (80 E-150 E) -- 8.2.2 The west (30 E-80 E) -- 8.3 Ecosystem change off east antarctica -- Summary -- References -- 9 THE DYNAMIC MOSAIC -- 9.1 Introduction -- 9.2 Historical and geographic perspectives -- 9.3 Disturbance -- 9.3.1 Ice effects -- 9.3.2 Asteroid impacts -- 9.3.3 Sediment instability and hypoxia -- 9.3.4 Wind and wave action -- 9.3.5 Pollution -- 9.3.6 UV irradiation. , 9.3.7 Volcanic eruptions -- 9.3.8 Trawling -- 9.3.9 Non-indigenous species (NIS) -- 9.3.10 Freshwater -- 9.3.11 Temperature stress -- 9.3.12 Biological agents of physical disturbance -- 9.4 Colonisaton of antarctic sea-beds -- 9.4.1 Larval abundance -- 9.4.2 Hard substrata -- 9.4.3 Soft sediments -- 9.5 Implications of climate change -- 9.6 Conclusion -- Acknowledgements -- References -- 10 SOUTHERN OCEAN DEEP BENTHIC BIODIVERSITY -- 10.1 Introduction -- 10.2 History of antarctic biodiversity work -- 10.3 Geological history and evolution of the antarctic -- 10.3.1 Indian Ocean -- 10.3.2 South Atlantic -- 10.3.3 Weddell Sea -- 10.3.4 Drake Passage and Scotia Sea -- 10.4 Benthic composition and diversity of meio-, macro- and megabenthos -- 10.4.1 Meiofauna -- 10.4.2 Macrofaunal composition and diversity -- 10.4.3 Megafaunal composition and diversity -- 10.5 Phylogenetic relationships of selected taxa -- 10.5.1 Foraminifera -- 10.5.2 Isopoda -- 10.5.3 Tanaidacea -- 10.5.4 Bivalvia -- 10.5.5 Polychaeta -- 10.5.6 Cephalopoda -- 10.6 Biogeography and endemism -- 10.6.1 Porifera -- 10.6.2 Foraminifera -- 10.6.3 Metazoan meiofauna -- 10.6.4 Peracarida -- 10.6.5 Mollusca -- 10.6.6 Echinodermata -- 10.6.7 Brachiopoda -- 10.6.8 Polychaeta -- 10.6.9 Bryozoa -- 10.7 Relationship of selected faunal assemblages to environmental variables -- 10.7.1 Large-scale patterns with depth -- 10.7.2 Patterns influenced by other environmental or physical factors -- 10.7.3 Isopoda -- 10.8 Similarities and differences between antarctic and other deep-sea systems -- 10.8.1 The environment -- 10.8.2 A direct comparison between the deep sea of the SO and the World Ocean -- 10.8.3 Dispersal and recruitment between the SO and the rest of the world -- 10.8.4 The special case of chemosynthetically-driven deep-sea systems -- 10.9 Conclusions -- Acknowledgements -- References. , 11 ENVIRONMENTAL FORCING AND SOUTHERN OCEAN MARINE PREDATOR POPULATIONS -- 11.1 Climate change: recent, rapid, regional warming -- 11.2 Using oscillatory climate signals to predict future change in biological communities -- 11.3 Potential for regional impacts on the biosphere -- 11.4 Confounding isues in identifying a biological signal -- 11.5 Regional ecosystem responses as a consequence of variation in regional food webs -- 11.6 Where biological signals will be most apparent -- 11.7 The southwest atlantic -- 11.8 The indian ocean -- 11.9 The pacific ocean -- 11.10 Similarities between the atlantic, indian and pacific oceans -- 11.11 What ENSO can tell us -- 11.12 Future scenarios -- References -- PART 3: MOLECULAR ADAPTATIONS AND EVOLUTION -- 12 MOLECULAR ECOPHYSIOLOGY OF ANTARCTIC NOTOTHENIOID FISHES* -- 12.1 Introduction -- 12.2 Surviving the big chill - notothenioid freezing avoidance by antifreeze proteins -- 12.2.1 Freezing challenge in frigid Antarctic marine environment -- 12.2.2 Historical paradigm of teleost freezing avoidance -- 12.2.3 Paradigm shift I: the 'larval paradox' -- 12.2.4 Paradigm shift II: liver is not the source of blood AFGP in notothenioids -- 12.2.5 Gut versus blood - importance of intestinal freeze avoidance -- 12.2.6 Non-hepatic source of plasma AFGP -- 12.2.7 Alterations in environments and dynamic evolutionary change in notothenioid AFGP gene families -- 12.2.8 Summary comments - antifreeze protein gain in Antarctic notothenioid fish -- 12.3 Haemoprotein loss and cardiovascular adaptation in icefishes - dr. no to the rescue? -- 12.3.1 Vertebrates without haemoglobins - you must be kidding! -- 12.3.2 Haemoprotein loss in icefishes: an evolutionary perspective -- 12.3.3 Cellular correlates of haemoprotein loss -- 12.3.4 The icefish cardiovascular system. , 12.3.5 Compensatory adjustment of the icefish cardiovascular system in a regime of reduced interspecific competition? Enter Dr. NO.
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  • 2
    Publication Date: 2022-05-25
    Description: © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in PLoS Biology 10 (2012): e1001234, doi:10.1371/journal.pbio.1001234.
    Description: Since the first discovery of deep-sea hydrothermal vents along the Galápagos Rift in 1977, numerous vent sites and endemic faunal assemblages have been found along mid-ocean ridges and back-arc basins at low to mid latitudes. These discoveries have suggested the existence of separate biogeographic provinces in the Atlantic and the North West Pacific, the existence of a province including the South West Pacific and Indian Ocean, and a separation of the North East Pacific, North East Pacific Rise, and South East Pacific Rise. The Southern Ocean is known to be a region of high deep-sea species diversity and centre of origin for the global deep-sea fauna. It has also been proposed as a gateway connecting hydrothermal vents in different oceans but is little explored because of extreme conditions. Since 2009 we have explored two segments of the East Scotia Ridge (ESR) in the Southern Ocean using a remotely operated vehicle. In each segment we located deep-sea hydrothermal vents hosting high-temperature black smokers up to 382.8°C and diffuse venting. The chemosynthetic ecosystems hosted by these vents are dominated by a new yeti crab (Kiwa n. sp.), stalked barnacles, limpets, peltospiroid gastropods, anemones, and a predatory sea star. Taxa abundant in vent ecosystems in other oceans, including polychaete worms (Siboglinidae), bathymodiolid mussels, and alvinocaridid shrimps, are absent from the ESR vents. These groups, except the Siboglinidae, possess planktotrophic larvae, rare in Antarctic marine invertebrates, suggesting that the environmental conditions of the Southern Ocean may act as a dispersal filter for vent taxa. Evidence from the distinctive fauna, the unique community structure, and multivariate analyses suggest that the Antarctic vent ecosystems represent a new vent biogeographic province. However, multivariate analyses of species present at the ESR and at other deep-sea hydrothermal vents globally indicate that vent biogeography is more complex than previously recognised.
    Description: The ChEsSo research programme was funded by a NERC Consortium Grant (NE/DO1249X/1) and supported by the Census of Marine Life and the Sloan Foundation, and the Total Foundation for Biodiversity (Abyss 2100)(SVTH) all of which are gratefully acknowledged. We also acknowledge NSF grant ANT-0739675 (CG and TS), NERC PhD studentships NE/D01429X/1(LH, LM, CNR), NE/H524922/1(JH) and NE/F010664/1 (WDKR), a Cusanuswerk doctoral fellowship, and a Lesley & Charles Hilton-Brown Scholarship, University of St. Andrews (PHBS).
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 3
    Publication Date: 2022-05-26
    Description: © The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 4 (2014): 5024, doi:10.1038/srep05024.
    Description: Climate change is a major threat to global biodiversity. Antarctic ecosystems are no exception. Investigating past species responses to climatic events can distinguish natural from anthropogenic impacts. Climate change produces ‘winners’, species that benefit from these events and ‘losers’, species that decline or become extinct. Using molecular techniques, we assess the demographic history and population structure of Pygoscelis penguins in the Scotia Arc related to climate warming after the Last Glacial Maximum (LGM). All three pygoscelid penguins responded positively to post-LGM warming by expanding from glacial refugia, with those breeding at higher latitudes expanding most. Northern (Pygoscelis papua papua) and Southern (Pygoscelis papua ellsworthii) gentoo sub-species likely diverged during the LGM. Comparing historical responses with the literature on current trends, we see Southern gentoo penguins are responding to current warming as they did during post-LGM warming, expanding their range southwards. Conversely, Adélie and chinstrap penguins are experiencing a ‘reversal of fortunes’ as they are now declining in the Antarctic Peninsula, the opposite of their response to post-LGM warming. This suggests current climate warming has decoupled historic population responses in the Antarctic Peninsula, favoring generalist gentoo penguins as climate change ‘winners’, while Adélie and chinstrap penguins have become climate change ‘losers’.
    Description: We thank the Zoological Society of London, Quark Expeditions, Exodus Travels ltd., Oceanites, the Holly Hill Charitable Trust, the Charities Advisory Trust and an U.S. National Science Foundation (NSF) Office of Polar Programs grant (ANT-0739575) for funding.
    Keywords: Climate-change ecology ; Molecular ecology ; Molecular evolution ; Population genetics
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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