Projected changes of Antarctic krill habitat by the end of the 21st century

Climate change is rapidly shaping the living environment of the most abundant keystone species of the Antarctic marine food web, Antarctic krill. Projected future changes for the krill habitat include a sustained increase in ocean temperature and changes in sea ice and chlorophyll a. Here we investigate how these factors affect the early life history of krill and identify the regions around Antarctica where the impact will be greatest. Our tool is a temperature-dependent krill growth model forced by data from comprehensive greenhouse warming simulations. We find that by the year 2100 localized regions along the western Weddell Sea, isolated areas of the Indian Antarctic , and the Amundsen/Bellingshausen Sea will support successful spawning habitats for krill. The failure of potentially successful spawning will have a strong impact on the already declining adult populations with consequences for the Antarctic marine food web, having both ecological and commercial ramifications.

[1]  S. Sokolov,et al.  Circumpolar structure and distribution of the Antarctic Circumpolar Current fronts: 1. Mean circumpolar paths , 2009 .

[2]  E. Hofmann,et al.  Sensitivity of Circumpolar Deep Water Transport and Ice Shelf Basal Melt along the West Antarctic Peninsula to Changes in the Winds , 2012 .

[3]  S. Stammerjohn,et al.  Trends in Antarctic annual sea ice retreat and advance and their relation to El Niño–Southern Oscillation and Southern Annular Mode variability , 2008 .

[4]  Donald J. Cavalieri,et al.  Arctic and Antarctic Sea Ice, 1978-1987: Satellite Passive-Microwave Observations and Analysis , 1992 .

[5]  A. Ishida,et al.  Risk maps for Antarctic krill under projected Southern Ocean acidification , 2013 .

[6]  E. Hofmann,et al.  Modeling the remote and local connectivity of Antarctic Krill Populations along the Western Antarctic Peninsula , 2013 .

[7]  E. Murphy,et al.  Natural growth rates in Antarctic krill (Euphausia superba): I. Improving methodology and predicting intermolt period , 2006 .

[8]  M. H. Duong,et al.  Integrated Risk and Uncertainty Assessment of Climate Change Response Policies , 2014 .

[9]  E. Pakhomova,et al.  Daily rations and growth of larval krill Euphausia superba in the Eastern Bellingshausen Sea during austral autumn , 2004 .

[10]  L. Quetin,et al.  Episodic recruitment in Antarctic krill Euphausia superba in the Palmer LTER study region , 2003 .

[11]  M. Brandon,et al.  Tracking passive drifters in a high resolution ocean model: implications for interannual variability of larval krill transport to South Georgia , 2004 .

[12]  S. Doney,et al.  Biological ramifications of climate-change-mediated oceanic multi-stressors , 2015 .

[13]  Gene E. Likens,et al.  Trends in stream nitrogen concentrations for forested reference catchments across the USA , 2013 .

[14]  Christoph Heinze,et al.  Multiple stressors of ocean ecosystems in the 21st century: projections with CMIP5 models , 2013 .

[15]  S. Gille Warming of the Southern Ocean Since the 1950s , 2002, Science.

[16]  N. Nakicenovic,et al.  RCP 8.5—A scenario of comparatively high greenhouse gas emissions , 2011 .

[17]  B. Meyer,et al.  Feeding and energy budgets of Antarctic krill Euphausia superba at the onset of winter—I. Furcilia III larvae , 2002 .

[18]  Zhaomin Wang On the response of Southern Hemisphere subpolar gyres to climate change in coupled climate models , 2013 .

[19]  L. Quetin,et al.  Effect of temperature on developmental times and survival of early larval stages of Euphausia superba Dana , 1988 .

[20]  L. Quetin,et al.  Energetic cost to develop to the first feeding stage of Euphausia superba Dana and the effect of delays in food availability , 1989 .

[21]  J. Turner,et al.  An Initial Assessment of Antarctic Sea Ice Extent in the CMIP5 Models , 2013 .

[22]  M. Vernet,et al.  Ecological responses of Antarctic krill to environmental variability: can we predict the future? , 2007, Antarctic Science.

[23]  A. Atkinson,et al.  Potential Climate Change Effects on the Habitat of Antarctic Krill in the Weddell Quadrant of the Southern Ocean , 2013, PloS one.

[24]  E. Hofmann,et al.  Models of the early life history of Euphausia superba—Part I. Time and temperature dependence during the descent-ascent cycle , 1992 .

[25]  E. Murphy,et al.  Modeling Studies of Antarctic Krill ( Euphausia superba ) Survival During Transport Across the Scotia Sea and Environs , 2003 .

[26]  J. Marr The natural history and geography of the Antarctic krill (Euphausia superba Dana) , 1961 .

[27]  E. Murphy,et al.  Transport of Antarctic krill (Euphausia superba) across the Scotia Sea. Part II: Krill growth and survival , 2006 .

[28]  V. Siegel Distribution and population dynamics of Euphausia superba: summary of recent findings , 2005, Polar Biology.

[29]  K. Arrigo,et al.  Primary production in the Southern Ocean, 1997–2006 , 2008 .

[30]  E. Murphy,et al.  Circumpolar connections between Antarctic krill (Euphausia superba Dana) populations: investigating the roles of ocean and sea ice transport , 2007 .

[31]  Watson W. Gregg,et al.  Ocean primary production and climate: Global decadal changes , 2003 .

[32]  Robert J. Nicholls,et al.  How Do Polar Marine Ecosystems Respond to Rapid Climate Change , 2010 .

[33]  B. Meyer The overwintering of Antarctic krill, Euphausia superba, from an ecophysiological perspective , 2011, Polar Biology.

[34]  T. Roy,et al.  Assessment of Southern Ocean water mass circulation and characteristics in CMIP5 models: Historical bias and forcing response , 2013 .

[35]  E. Murphy,et al.  Life history buffering in Antarctic mammals and birds against changing patterns of climate and environmental variation , 2008 .

[36]  E. Murphy,et al.  Oceanic circumpolar habitats of Antarctic krill , 2008 .

[37]  S. Stammerjohn,et al.  Recent Changes in Phytoplankton Communities Associated with Rapid Regional Climate Change Along the Western Antarctic Peninsula , 2009, Science.

[38]  H. Schellnhuber,et al.  Decomposing the effects of ocean warming on chlorophyll a concentrations into physically and biologically driven contributions , 2013 .

[39]  B. Meyer,et al.  Physiology, growth, and development of larval krill Euphausia superba in autumn and winter in the Lazarev Sea, Antarctica , 2009 .

[40]  L. Quetin,et al.  Depth distribution of developing Euphausia superba embryos, predicted from sinking rates , 1984 .

[41]  E. Murphy,et al.  A foodweb model to explore uncertainties in the South Georgia shelf pelagic ecosystem , 2012 .

[42]  Peter Rothery,et al.  Natural growth rates in Antarctic krill (Euphausia superba): II. Predictive models based on food, temperature, body length, sex, and maturity stage , 2006 .

[43]  E. Hofmann,et al.  A circumpolar modeling study of habitat control of Antarctic krill (Euphausia superba) reproductive success , 2003 .

[44]  B. Meyer,et al.  Daily rations and growth of larval krill Euphausia superba in the Eastern Bellingshausen Sea during austral autumn , 2004 .

[45]  K. Daly Overwintering development, growth, and feeding of larval Euphausia superba in the Antarctic marginal ice zone , 1990 .

[46]  L. Quetin,et al.  Environmental Variability and Its Impact on the Reproductive Cycle of Antarctic Krill1 , 2001 .

[47]  A. Lombana,et al.  Impact of climate change on Antarctic krill , 2018 .

[48]  M. Long,et al.  Synergistic effects of iron and temperature on Antarctic phytoplankton and microzooplankton assemblages , 2009 .

[49]  A. Thomson,et al.  The representative concentration pathways: an overview , 2011 .

[50]  Peter Rothery,et al.  Long-term decline in krill stock and increase in salps within the Southern Ocean , 2004, Nature.

[51]  Walker O. Smith,et al.  Productivity and linkages of the food web of the southern region of the western Antarctic Peninsula continental shelf , 2014 .

[52]  T. Bracegirdle,et al.  Assessment of Southern Ocean mixed-layer depths in CMIP5 models: Historical bias and forcing response , 2013 .