FN Archimer Export Format
PT J
TI Biomass changes and trophic amplification of plankton in a warmer ocean
BT 
AF CHUST, Guillem
   ALLEN, J. Icarus
   BOPP, Laurent
   SCHRUM, Corinna
   HOLT, Jason
   TSIARAS, Kostas
   ZAVATARELLI, Marco
   CHIFFLET, Marina
   CANNABY, Heather
   DADOU, Isabelle
   DAEWEL, Ute
   WAKELIN, Sarah L.
   MACHU, Eric
   PUSHPADAS, Dhanya
   BUTENSCHON, Momme
   ARTIOLI, Yuri
   PETIHAKIS, Georges
   SMITH, Chris
   GARCON, Veronique
   GOUBANOVA, Katerina
   LE VU, Briac
   FACH, Bettina A.
   SALIHOGLU, Baris
   CLEMENTI, Emanuela
   IRIGOIEN, Xabier
AS 1:1;2:2;3:3;4:4;5:5;6:6;7:7,8;8:1;9:5,9;10:10;11:4,11;12:5;13:12;14:4;15:2;16:2;17:6;18:6;19:10;20:;21:10;22:9,10;23:9;24:1,8;25:13;
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C1 AZTI Tecnalia, Div Marine Res, Pasaia 20110, Spain.
   PML, Plymouth PL1 3DH, Devon, England.
   IPSL, LSCE, F-91191 Gif Sur Yvette, France.
   Univ Bergen GFI UIB, Inst Geophys, N-5007 Bergen, Norway.
   Natl Oceanog Ctr, Liverpool L3 5DA, Merseyside, England.
   HCMR, Mavro Lithari 19013, Anavyssos, Greece.
   Alma Mater Studiorum Univ Bologna, Dipartimento Fis & Astron, I-40127 Bologna, Italy.
   Alma Mater Studiorum Univ Bologna Sede Ravenna, Ctr Interdipartimentale Ric Sci Ambientali, I-48123 Ravenna, Italy.
   METU, Inst Marine Sci, TR-33731 Erdemli Mersin, Turkey.
   UPS, CNRS, CNES, LEGOS,IRD,OMP,UMR5566, F-31400 Toulouse, France.
   Nansen Environm & Remote Sensing Ctr, N-5006 Bergen, Norway.
   UBO, IRD, IFREMER, CNRS,Lab Phys Oceans,UMR6523, F-29280 Plouzane, France.
   KAUST, Red Sea Res Ctr, Thuwal 239556900, Saudi Arabia.
C2 AZTI, SPAIN
   PML, UK
   IPSL, FRANCE
   UNIV BERGEN, NORWAY
   NOC, UK
   HELLENIC CTR MARINE RES, GREECE
   UNIV BOLOGNA, ITALY
   UNIV BOLOGNA, ITALY
   METU, TURKEY
   UNIV TOULOUSE, FRANCE
   NERSC, NORWAY
   UBO, FRANCE
   UNIV KING ABDULLAH, SAUDI ARABIA
IF 8.044
TC 152
UR https://archimer.ifremer.fr/doc/00188/29966/28481.pdf
LA English
DT Article
DE ;ecosystem model;food web;plankton;primary production;sea warming;trophic amplification
AB Ocean warming can modify the ecophysiology and distribution of marine organisms, and relationships between species, with nonlinear interactions between ecosystem components potentially resulting in trophic amplification. Trophic amplification (or attenuation) describe the propagation of a hydroclimatic signal up the food web, causing magnification (or depression) of biomass values along one or more trophic pathways. We have employed 3-D coupled physical-biogeochemical models to explore ecosystem responses to climate change with a focus on trophic amplification. The response of phytoplankton and zooplankton to global climate-change projections, carried out with the IPSL Earth System Model by the end of the century, is analysed at global and regional basis, including European seas (NE Atlantic, Barents Sea, Baltic Sea, Black Sea, Bay of Biscay, Adriatic Sea, Aegean Sea) and the Eastern Boundary Upwelling System (Benguela). Results indicate that globally and in Atlantic Margin and North Sea, increased ocean stratification causes primary production and zooplankton biomass to decrease in response to a warming climate, whilst in the Barents, Baltic and Black Seas, primary production and zooplankton biomass increase. Projected warming characterized by an increase in sea surface temperature of 2.29 ± 0.05 °C leads to a reduction in zooplankton and phytoplankton biomasses of 11% and 6%, respectively. This suggests negative amplification of climate driven modifications of trophic level biomass through bottom-up control, leading to a reduced capacity of oceans to regulate climate through the biological carbon pump. Simulations suggest negative amplification is the dominant response across 47% of the ocean surface and prevails in the tropical oceans; whilst positive trophic amplification prevails in the Arctic and Antarctic oceans. Trophic attenuation is projected in temperate seas. Uncertainties in ocean plankton projections, associated to the use of single global and regional models, imply the need for caution when extending these considerations into higher trophic levels.
PY 2014
PD JUN
SO Global Change Biology
SN 1354-1013
PU Wiley-blackwell
VL 20
IS 7
UT 000337680700010
BP 2124
EP 2139
DI 10.1111/gcb.12562
ID 29966
ER

EF