Implications of dietary carbon incorporation in fish carbonates for the global carbon cycle

被引:0
|
作者
Oehlert, Amanda M. [1 ]
Garza, Jazmin [1 ]
Nixon, Sandy [2 ]
Frank, Leeann [2 ]
Folkerts, Erik J. [2 ]
Stieglitz, John D. [2 ]
Lu, Chaojin [1 ]
Heuer, Rachael M. [2 ]
Benetti, Daniel D. [2 ]
del Campo, Javier [2 ,3 ]
Gomez, Fabian A. [4 ,5 ]
Grosell, Martin [2 ]
机构
[1] Univ Miami, Rosenstiel Sch Marine Atmospher & Earth Sci, Dept Marine Geosci, Coral Gables, FL 33146 USA
[2] Univ Miami, Rosenstiel Sch Marine Atmospher & Earth Sci, Dept Marine Biol & Ecol, Coral Gables, FL USA
[3] Univ Pompeu Fabra, Inst Biol Evolut, CSIC, Barcelona, Spain
[4] Mississippi State Univ, Northern Gulf Inst, Mississippi State, MS USA
[5] NOAA Atlantic Oceanog & Meteorol Lab, Miami, FL USA
基金
美国国家科学基金会;
关键词
Global carbon cycle; Marine fish; Osmoregulation; Biological pump; Carbonate pump; Stable carbon isotope ratios; COBIA RACHYCENTRON-CANADUM; INTESTINAL BICARBONATE SECRETION; MARINE TELEOST FISH; METABOLIC-RATE; RAINBOW-TROUT; FECAL PELLETS; FRACTIONATION; ISOTOPES; PTEROPODS; MAGNESIUM;
D O I
10.1016/j.scitotenv.2024.169895
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Marine bony fish are important participants in Earth's carbon cycle through their contributions to the biological pump and the marine inorganic carbon cycle. However, uncertainties in the composition and magnitude of fish contributions preclude their integration into fully coupled carbon-climate models. Here, we consider recent upwards revisions to global fish biomass estimates (2.7-9.5x) and provide new stable carbon isotope measurements that show marine fish are prodigious producers of carbonate with unique composition. Assuming the median increase (4.17x) in fish biomass estimates is linearly reflected in fish carbonate (ichthyocarbonate) production rate, marine fish are estimated to produce between 1.43 and 3.99 Pg CaCO3 yr(-1), but potentially as much as 9.03 Pg CaCO3 yr(-1). Thus, marine fish carbonate production is equivalent to or potentially higher than contributions by coccolithophores or pelagic foraminifera. New stable carbon isotope analyses indicate that a significant proportion of ichthyocarbonate is derived from dietary carbon, rather than seawater dissolved inorganic carbon. Using a statistical mixing model to derive source contributions, we estimate ichthyocarbonate contains up to 81 % dietary carbon, with average compositions of 28-56 %, standing in contrast to contents <10 % in other biogenic carbonate minerals. Results also indicate ichthyocarbonate contains 5.5-40.4 % total organic carbon. When scaled to the median revised global production of ichthyocarbonate, an additional 0.08 to 1.61 Pg C yr(-1) can potentially be added to estimates of fish contributions to the biological pump, significantly increasing marine fish contributions to total surface carbon export. Our integration of geochemical and physiological analyses identifies an overlooked link between carbonate production and the biological pump. Since ichthyocarbonate production is anticipated to increase with climate change scenarios, due to ocean warming and acidification, these results emphasize the importance of quantitative understanding of the multifaceted role of marine fish in the global carbon cycle.
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页数:13
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