Climate change and glacier retreat drive shifts in an Antarctic benthic ecosystem

The Antarctic Peninsula (AP) is one of the three places on Earth that registered the most intense warming in the last 50 years, almost five times the global mean. This warming has strongly affected the cryosphere, causing the largest ice-shelf collapses ever observed and the retreat of 87% of glacie...

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Autor principal: Sahade, R.
Otros Autores: Lagger, C., Torre, L., Momo, F., Monien, P., Schloss, I., Barnes, D.K.A, Servetto, N., Tarantelli, S., Tatián, M., Zamboni, N., Abele, D.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: American Association for the Advancement of Science 2015
Acceso en línea:Registro en Scopus
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100 1 |a Sahade, R. 
245 1 0 |a Climate change and glacier retreat drive shifts in an Antarctic benthic ecosystem 
260 |b American Association for the Advancement of Science  |c 2015 
270 1 0 |m Sahade, R.; Inst. de Diversidad y Ecologia Animal Consejo Nacional de Investigaciones Cientificas y Tecnicas, Universidad Nacional de Córdoba (CONICET-UNC), Facultad de Ciencias Exactas, Físicas y Naturales, UNC, Avenida Vélez Sarsfield 299, Argentina; email: rsahade@efn.uncor.edu 
506 |2 openaire  |e Política editorial 
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520 3 |a The Antarctic Peninsula (AP) is one of the three places on Earth that registered the most intense warming in the last 50 years, almost five times the global mean. This warming has strongly affected the cryosphere, causing the largest ice-shelf collapses ever observed and the retreat of 87% of glaciers. Ecosystem responses, although increasingly predicted, have been mainly reported for pelagic systems. However, and despite most Antarctic species being benthic, responses in the Antarctic benthos have been detected in only a few species, and major effects at assemblage level are unknown. This is probably due to the scarcity of baselines against which to assess change. We performed repeat surveys of coastal benthos in 1994, 1998, and 2010, analyzing community structure and environmental variables at King George Island, Antarctica. We report a marked shift in an Antarctic benthic community that can be linked to ongoing climate change. However, rather than temperature as the primary factor, we highlight the resulting increased sediment runoff, triggered by glacier retreat, as the potential causal factor. The sudden shift from a "filter feeders-ascidian domination" to a "mixed assemblage" suggests that thresholds (for example, of tolerable sedimentation) and alternative equilibrium states, depending on the reversibility of the changes, could be possible traits of this ecosystem. Sedimentation processes will be increasing under the current scenario of glacier retreat, and attention needs to be paid to its effects along the AP. © 2015 The Authors.  |l eng 
536 |a Detalles de la financiación: 2Instituto, UNC, University of North Carolina 
536 |a Detalles de la financiación: FCFM, Facultad de Ciencias Físicas y Matemáticas 
536 |a Detalles de la financiación: CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas 
536 |a Detalles de la financiación: NERC, Natural Environment Research Council 
536 |a Detalles de la financiación: 5Department 
536 |a Detalles de la financiación: AWI, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research 
536 |a Detalles de la financiación: Universität Bremen 
536 |a Detalles de la financiación: 1Instituto de Diversidad y Ecología Animal [Consejo Nacional de Investigaciones Científicas y Técnicas–Universidad Nacional de Córdoba (CONICET-UNC)], Facultad de Ciencias Exactas, Físicas y Naturales, UNC, Avenida Vélez Sarsfield 299, 5000 Córdoba, Argentina. 2Instituto de Ciencias, Universidad Nacional de General Sarmiento, Juan M. Gutiérrez 1150, B1613GSX Los Polvorines, Argentina. 3Instituto de Ecología y Desarrollo Sustentable, Universidad Nacional de Luján, Luján 6700, Argentina. 4Institute for Chemistry and Biology of the Marine Environment, Carl-von-Ossietzky Straße 9-11, 26129 Oldenburg, Germany. 5Department of Geosciences, University of Bremen, Klagenfurter Straße (GEO), 28359 Bremen, Germany. 6Instituto Antártico Argentino, Balcarce 290, Ciudad Autónoma de Buenos Aires C1064AAF, Argentina. 7British Antarctic Survey, Natural Environment Research Council, Madingley, Road, Cambridge CB3 0ET, UK. 8Alfred Wegener Institut for Polar and Marine Research, Columbusstraße, 27568 Bremerhaven, Germany. *Corresponding author. E-mail: rsahade@efn.uncor.edu 
593 |a Inst. de Diversidad y Ecologia Animal Consejo Nacional de Investigaciones Cientificas y Tecnicas, Universidad Nacional de Córdoba (CONICET-UNC), Facultad de Ciencias Exactas, Físicas y Naturales, UNC, Avenida Vélez Sarsfield 299, Córdoba, Argentina 
593 |a Instituto de Ciencias, Universidad Nacional de General Sarmiento, Juan M. Gutiérrez 1150, Los Polvorines, Argentina 
593 |a Instituto de Ecología y Desarrollo Sustentable, Universidad Nacional de Luján, Luján, Argentina 
593 |a Institute for Chemistry and Biology of the Marine Environment, Carl-von-Ossietzky Straße 9-11, Oldenburg, Germany 
593 |a Department of Geosciences, University of Bremen, Klagenfurter Straße (GEO), Bremen, Germany 
593 |a Instituto Antártico Argentino, Balcarce 290, Ciudad Autónoma de Buenos Aires, Argentina 
593 |a British Antarctic Survey, Natural Environment Research Council, Madingley Road, Cambridge, United Kingdom 
593 |a Alfred Wegener Institut for Polar and Marine Research, Columbusstraße, Bremerhaven, Germany 
690 1 0 |a ECOLOGY 
690 1 0 |a ECOSYSTEMS 
690 1 0 |a ANTARCTIC BENTHOS 
690 1 0 |a ANTARCTIC PENINSULA 
690 1 0 |a BENTHIC COMMUNITIES 
690 1 0 |a BENTHIC ECOSYSTEMS 
690 1 0 |a COMMUNITY STRUCTURES 
690 1 0 |a ECOSYSTEM RESPONSE 
690 1 0 |a ENVIRONMENTAL VARIABLES 
690 1 0 |a SEDIMENTATION PROCESS 
690 1 0 |a CLIMATE CHANGE 
700 1 |a Lagger, C. 
700 1 |a Torre, L. 
700 1 |a Momo, F. 
700 1 |a Monien, P. 
700 1 |a Schloss, I. 
700 1 |a Barnes, D.K.A. 
700 1 |a Servetto, N. 
700 1 |a Tarantelli, S. 
700 1 |a Tatián, M. 
700 1 |a Zamboni, N. 
700 1 |a Abele, D. 
773 0 |d American Association for the Advancement of Science, 2015  |g v. 1  |k n. 10  |x 23752548  |t Sci. Adv. 
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