Climate change and the oceans - What does the future hold?

被引:161
作者
Bijma, Jelle [1 ]
Poertner, Hans-O [1 ]
Yesson, Chris [2 ]
Rogers, Alex D. [3 ]
机构
[1] Alfred Wegener Inst Polar & Marine Res, Bremerhaven, Germany
[2] Zool Soc London, Inst Zool, London NW1 4RY, England
[3] Univ Oxford, Dept Zool, Oxford OX1 3PS, England
关键词
EOCENE THERMAL MAXIMUM; PERMIAN MASS EXTINCTION; OXYGEN-MINIMUM ZONES; SOUTHERN-OCEAN; SEA-ICE; MARINE BIODIVERSITY; CORAL COMMUNITIES; DEEP-TIME; ACIDIFICATION; CARBON;
D O I
10.1016/j.marpolbul.2013.07.022
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The ocean has been shielding the earth from the worst effects of rapid climate change by absorbing excess carbon dioxide from the atmosphere. This absorption of CO2 is driving the ocean along the pH gradient towards more acidic conditions. At the same time ocean warming is having pronounced impacts on the composition, structure and functions of marine ecosystems. Warming, freshening (in some areas) and associated stratification are driving a trend in ocean deoxygenation, which is being enhanced in parts of the coastal zone by upwelling of hypoxic deep water. The combined impact of warming, acidification and deoxygenation are already having a dramatic effect on the flora and fauna of the oceans with significant changes in distribution of populations, and decline of sensitive species. In many cases, the impacts of warming, acidification and deoxygenation are increased by the effects of other human impacts, such as pollution, eutrophication and overfishing. The interactive effects of this deadly trio mirrors similar events in the Earth's past, which were often coupled with extinctions of major species' groups. Here we review the observed impacts and, using past episodes in the Earth's history, set out what the future may hold if carbon emissions and climate change are not significantly reduced with more or less immediate effect. (C) 2013 Published by Elsevier Ltd.
引用
收藏
页码:495 / 505
页数:11
相关论文
共 144 条
[1]   Antarctic penguin response to habitat change as Earth's troposphere reaches 2°C above preindustrial levels [J].
Ainley, David ;
Russell, Joellen ;
Jenouvrier, Stephanie ;
Woehler, Eric ;
Lyver, Philip O'B ;
Fraser, William R. ;
Kooyman, Gerald L. .
ECOLOGICAL MONOGRAPHS, 2010, 80 (01) :49-66
[2]   End-Cretaceous marine mass extinction not caused by productivity collapse [J].
Alegret, Laia ;
Thomas, Ellen ;
Lohmann, Kyger C. .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2012, 109 (03) :728-732
[3]  
[Anonymous], 2007, CLIMATE CHANGE 2007
[4]  
[Anonymous], MAR POLLUT B
[5]  
[Anonymous], HOLOCENE EXTINCTIONS
[6]  
[Anonymous], CLIM CHANG 2007
[7]   Ocean acidification causes bleaching and productivity loss in coral reef builders [J].
Anthony, K. R. N. ;
Kline, D. I. ;
Diaz-Pulido, G. ;
Dove, S. ;
Hoegh-Guldberg, O. .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2008, 105 (45) :17442-17446
[8]   Impact of a shrinking Arctic ice cover on marine primary production [J].
Arrigo, Kevin R. ;
van Dijken, Gert ;
Pabi, Sudeshna .
GEOPHYSICAL RESEARCH LETTERS, 2008, 35 (19)
[9]  
Bambach RK, 2004, PALEOBIOLOGY, V30, P522, DOI 10.1666/0094-8373(2004)030<0522:OEAMDO>2.0.CO
[10]  
2