The imprint of anthropogenic CO2 emissions on Atlantic bluefin tuna otoliths

被引:12
|
作者
Fraile, Igaratza [1 ]
Arrizabalaga, Haritz [1 ]
Groeneveld, Jeroen [2 ]
Koelling, Martin [2 ]
Santos, Miguel Neves [3 ]
Macias, David [4 ]
Addis, Piero [5 ]
Dettman, David L. [6 ]
Karakulak, Saadet [7 ]
Deguara, Simeon [8 ]
Rooker, Jay R. [9 ]
机构
[1] AZTI Tecnalia, Div Marine Res, Pasaia 20110, Spain
[2] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany
[3] Inst Portugues Mar & Atmosfera IPMA IP, Ave 5 Outubro S-N, P-8700305 Olhao, Portugal
[4] Spanish Inst Oceanog, Corazon de Maria 8, Madrid 28002, Spain
[5] Univ Cagliari, Dept Life Sci & Environm, Via Fiorelli 1, I-09126 Cagliari, Italy
[6] Univ Arizona, Environm Isotope Lab, Dept Geosci, 1040 E 4th St, Tucson, AZ 85721 USA
[7] Istanbul Univ, Fac Fisheries, Ordu Cad 200, TR-34470 Istanbul, Turkey
[8] Federat Maltese Aquaculture Producers, 54 St Christopher Str, VLT-1462 Valletta, Malta
[9] Texas A&M Univ, Dept Marine Biol, 1001 Texas Clipper Rd, Galveston, TX 77553 USA
关键词
delta C-13 and delta O-18; Mediterranean Sea; CO2; emission; Suess effect; CARBON-ISOTOPE DISTRIBUTION; CLIMATE VARIABILITY; ATMOSPHERIC CO2; SURFACE OCEANS; RECENT TRENDS; DELTA C-13; SEA; EXCHANGE; OXYGEN; FISH;
D O I
10.1016/j.jmarsys.2015.12.012
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Otoliths of Atlantic bluefin tuna (Thunnus thynnus) collected from the Mediterranean Sea and North Atlantic Ocean were analyzed to evaluate changes in the seawater isotopic composition over time. We report an annual otolith delta C-13 record that documents the magnitude of the delta C-13 depletion in the Mediterranean Sea between 1989 and 2010. Atlantic bluefin tuna in our sample (n = 632) ranged from 1 to 22 years, and otolith material corresponding to the first year of life (back-calculated birth year) was used to reconstruct seawater isotopic composition. Otolith 8180 remained relatively stable between 1989 and 2010, whereas a statistically significant decrease in delta C-13 was detected across the time interval investigated, with a rate of decline of 0.05 parts per thousand yr(-1) (-0.94 parts per thousand depletion throughout the recorded period). The depletion in otolith delta C-13 over time was associated with the oceanic uptake of anthropogenically derived CO2. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:26 / 33
页数:8
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