GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 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.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2022-10-26
    Description: © The Author(s), 2020. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Howell, K. L., Hilario, A., Allcock, A. L., Bailey, D. M., Baker, M., Clark, M. R., Colaco, A., Copley, J., Cordes, E. E., Danovaro, R., Dissanayake, A., Escobar, E., Esquete, P., Gallagher, A. J., Gates, A. R., Gaudron, S. M., German, C. R., Gjerde, K. M., Higgs, N. D., Le Bris, N., Levin, L. A., Manea, E., McClain, C., Menot, L., Mestre, N. C., Metaxas, A., Milligan, R. J., Muthumbi, A. W. N., Narayanaswamy, B. E., Ramalho, S. P., Ramirez-Llodra, E., Robson, L. M., Rogers, A. D., Sellanes, J., Sigwart, J. D., Sink, K., Snelgrove, P. V. R., Stefanoudis, P., V., Sumida, P. Y., Taylor, M. L., Thurber, A. R., Vieira, R. P., Watanabe, H. K., Woodall, L. C., & Xavier, J. R. A blueprint for an inclusive, global deep-sea ocean decade field program. Frontiers in Marine Science, 7, (2020): 584861, doi:10.3389/fmars.2020.584861.
    Description: The ocean plays a crucial role in the functioning of the Earth System and in the provision of vital goods and services. The United Nations (UN) declared 2021–2030 as the UN Decade of Ocean Science for Sustainable Development. The Roadmap for the Ocean Decade aims to achieve six critical societal outcomes (SOs) by 2030, through the pursuit of four objectives (Os). It specifically recognizes the scarcity of biological data for deep-sea biomes, and challenges the global scientific community to conduct research to advance understanding of deep-sea ecosystems to inform sustainable management. In this paper, we map four key scientific questions identified by the academic community to the Ocean Decade SOs: (i) What is the diversity of life in the deep ocean? (ii) How are populations and habitats connected? (iii) What is the role of living organisms in ecosystem function and service provision? and (iv) How do species, communities, and ecosystems respond to disturbance? We then consider the design of a global-scale program to address these questions by reviewing key drivers of ecological pattern and process. We recommend using the following criteria to stratify a global survey design: biogeographic region, depth, horizontal distance, substrate type, high and low climate hazard, fished/unfished, near/far from sources of pollution, licensed/protected from industry activities. We consider both spatial and temporal surveys, and emphasize new biological data collection that prioritizes southern and polar latitudes, deeper (〉 2000 m) depths, and midwater environments. We provide guidance on observational, experimental, and monitoring needs for different benthic and pelagic ecosystems. We then review recent efforts to standardize biological data and specimen collection and archiving, making “sampling design to knowledge application” recommendations in the context of a new global program. We also review and comment on needs, and recommend actions, to develop capacity in deep-sea research; and the role of inclusivity - from accessing indigenous and local knowledge to the sharing of technologies - as part of such a global program. We discuss the concept of a new global deep-sea biological research program ‘Challenger 150,’ highlighting what it could deliver for the Ocean Decade and UN Sustainable Development Goal 14.
    Description: Development of this paper was supported by funding from the Scientific Committee on Oceanic Research (SCOR) awarded to KH and AH as working group 159 co-chairs. KH, BN, and KS are supported by the UKRI funded One Ocean Hub NE/S008950/1. AH work is supported by the CESAM (UIDP/50017/2020 + 1432 UIDB/50017/2020) that is funded by Fundação para a Ciência e a Tecnologia (FCT)/MCTES through national funds. AA is supported by Science Foundation Ireland and the Marine Institute under the Investigators Program Grant Number SFI/15/IA/3100 co-funded under the European Regional Development Fund 2014–2020. AC is supported through the FunAzores -ACORES 01-0145-FEDER-000123 grant and by FCT through strategic project UID/05634/2020 and FCT and Direção-Geral de Politica do Mar (DGPM) through the project Mining2/2017/005. PE is funded by national funds (OE), through FCT in the scope of the framework contract foreseen in the numbers 4, 5 and 6 of the article 23, of the Decree-Law 57/2016, of August 29, changed by Law 57/2017, of July 19. SG research is supported by CNRS funds. CG is supported by an Independent Study Award and the Investment in Science Fund at WHOI. KG gratefully acknowledges support from Synchronicity Earth. LL is funded by the NOAA Office of Ocean Exploration and Research (NA19OAR0110305) and the US National Science Foundation (OCE 1634172). NM is supported by FCT and DGPM, through the project Mining2/2017/001 and the FCT grants CEECIND/00526/2017, UIDB/00350/2020 + UIDP/00350/2020. SR is funded by the FCTgrant CEECIND/00758/2017. JS is supported by ANID FONDECYT #1181153 and ANID Millennium Science Initiative Program #NC120030. JX research is funded by the European Union’s Horizon 2020 research and innovation program through the SponGES project (grant agreement no. 679849) and further supported by national funds through FCT within the scope of UIDB/04423/2020 and UIDP/04423/2020. The Natural Sciences and Engineering Council of Canada supports AM and PVRS. MB and the Deep-Ocean Stewardship Initiative are supported by Arcadia - A charitable fund of Lisbet Rausing and Peter Baldwin. BN work is supported by the NERC funded Arctic PRIZE NE/P006302/1.
    Keywords: Deep sea ; Blue economy ; Ocean Decade ; Biodivercity ; Essential ocean variables
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...