Chemical and biological impacts of ocean acidification along the west coast of North America

被引:136
|
作者
Feely, Richard A. [1 ]
Alin, Simone R. [1 ]
Carter, Brendan [2 ]
Bednarsek, Nina [1 ,3 ]
Hales, Burke [4 ]
Chan, Francis [5 ]
Hill, Tessa M. [6 ,7 ]
Gaylord, Brian [6 ]
Sanford, Eric [6 ]
Byrne, Robert H. [8 ]
Sabine, Christopher L. [1 ]
Greeley, Dana [1 ]
Juranek, Lauren [4 ]
机构
[1] NOAA, Pacific Marine Environm Lab, 7600 Sand Point Way NE, Seattle, WA 98115 USA
[2] Univ Washington, Joint Inst Study Atmosphere & Ocean, Seattle, WA 98195 USA
[3] Univ Washington, Sch Marine & Environm Affairs, Seattle, WA 98195 USA
[4] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA
[5] Oregon State Univ, Dept Integrat Biol, Corvallis, OR 97331 USA
[6] Univ Calif Davis, Bodega Marine Lab, Bodega Bay, CA 94923 USA
[7] Univ Calif Davis, Dept Earth & Planetary Sci, Davis, CA 95616 USA
[8] Univ S Florida, Coll Marine Sci, 140 7th Ave South, St Petersburg, FL 33701 USA
基金
美国海洋和大气管理局; 美国国家科学基金会;
关键词
California current large marine ecosystem; Ocean acidification; Anthropogenic CO2; Upwelling; Pteropod dissolution; PACIFIC; CARBON; MARINE; CO2; SEAWATER; WATER; ARAGONITE; SYSTEM; PH; THERMODYNAMICS;
D O I
10.1016/j.ecss.2016.08.043
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
The continental shelf region off the west coast of North America is seasonally exposed to water with a low aragonite saturation state by coastal upwelling of CO2-rich waters. To date, the spatial and temporal distribution of anthropogenic CO2 (Canth) within the CO2-rich waters is largely unknown. Here we adapt the multiple linear regression approach to utilize the GO-SHIP Repeat Hydrography data from the northeast Pacific to establish an annually updated relationship between Canth and potential density. This relationship was then used with the NOAA Ocean Acidification Program West Coast Ocean Acidification (WCOA) cruise data sets from 2007, 2011, 2012, and 2013 to determine the spatial variations of Canth in the upwelled water. Our results show large spatial differences in Canth in surface waters along the coast, with the lowest values (37-55 limol kg(-1)) in strong upwelling regions off southern Oregon and northern California and higher values (51-63 limol kg(-1)) to the north and south of this region. Coastal dissolved inorganic carbon concentrations are also elevated due to a natural remineralized component (Cbio), which represents carbon accumulated through net respiration in the seawater that has not yet degassed to the atmosphere. Average surface Canth is almost twice the surface remineralized component. In contrast, Canth is only about one third and one fifth of the remineralized component at 50 m and 100 m depth, respectively. Uptake of Canth has caused the aragonite saturation horizon to shoal by approximately 30-50 m since the preindustrial period so that undersaturated waters are well within the regions of the continental shelf that affect the shell dissolution of living pteropods. Our data show that the most severe biological impacts occur in the nearshore waters, where corrosive waters are closest to the surface. Since the pre-industrial times, pteropod shell dissolution has, on average, increased approximately 19-26% in both nearshore and offshore waters. Published by Elsevier Ltd.
引用
收藏
页码:260 / 270
页数:11
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