Zoeken
Zoeken kan via de modus 'eenvoudig zoeken' (één veld) of uitgebreid via 'geavanceerd zoeken' (meerdere velden). Zo kan je bv. zoeken op een combinatie van een auteursnaam (auteur), een jaartal (jaar) en een documenttype.
Boekenmand
Nuttige resultaten kan je aanvinken en toevoegen aan een mandje. De inhoud hiervan kan je exporteren of afdrukken (naar bv. PDF).
RSS
Op de hoogte blijven van nieuw toegevoegde publicaties binnen uw interessegebied? Dit kan door een RSS-feed (?) te maken van jouw zoekopdracht.
nieuwe zoekopdracht
Climate change and glacier retreat drive shifts in an Antarctic benthic ecosystem
Sahade, R.; Lagger, C.; Torre, L.; Momo, F.R.; Monien, P.; Schloss, I.; Barnes, D.K.A.; Servetto, N.; Tarantelli, S.; Tatián, M.; Zamboni, N.; Abele, D. (2015). Climate change and glacier retreat drive shifts in an Antarctic benthic ecosystem. Science Advances 1(10): 8 pp. http://dx.doi.org/10.1126/sciadv.1500050
In: Science Advances. AAAS: New York. ISSN 2375-2548; e-ISSN 2375-2548
| |
| Auteurs | | Top |
- Sahade, R.
- Lagger, C.
- Torre, L.
- Momo, F.R.
|
- Monien, P.
- Schloss, I.
- Barnes, D.K.A.
- Servetto, N.
|
- Tarantelli, S.
- Tatián, M.
- Zamboni, N.
- Abele, D.
|
| Abstract |
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. |
IMIS is ontwikkeld en wordt gehost door het VLIZ.