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Significant carbonate burial in The Bahamas seagrass ecosystem

Bibliographic Data

ID15545858
AuthorsChuancheng Fu (0000-0001-5982-6809, King Abdullah University of Science and Technology, corresponding author), Sofia Frappi (0000-0002-0184-5537, King Abdullah University of Science and Technology), Michelle-Nicole Havlik (0000-0001-5535-4189, King Abdullah University of Science and Technology), Wells Howe (0000-0003-0464-7461), S David Harris (0009-0006-3933-2522), Elisa Laiolo (0000-0002-6107-0454, King Abdullah University of Science and Technology), Austin J Gallagher (0000-0003-1515-3440), Pere Masqué (0000-0002-1789-320X, Edith Cowan University), Carlos M Duarte (0000-0002-1213-1361, King Abdullah University of Science and Technology)
Year2024
Volume19
Issue9
Pages094036-094036
Publication date2024-08-01
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ad6a29
OpenAlexW4401205803
LanguageEN
References cited2

Seagrass meadows store significant amounts of carbonate (CaCO 3 ) in sediment, contributing to coastal protection but potentially offsetting their effectiveness as carbon sinks. Understanding the accumulation of CaCO 3 and its balance with organic carbon (C org ) in seagrass ecosystems is crucial for developing seagrass-based blue carbon strategies for climate change mitigation. However, CaCO 3 accumulation in seagrass meadows varies significantly across geographic regions, with notable data gaps in the Caribbean and Central America. Here, we sampled 10 seagrass meadows across an extensive island chain in The Bahamas, part of the largest seagrass ecosystem and one of the largest CaCO 3 banks globally, to evaluate CaCO 3 stock, accumulation rate, and its balance with C org sequestration. Seagrass meadows in The Bahamas store 6405–8847 Tg of inorganic carbon (C inorg ) in the upper meter sediment, with an annual accumulation rate of 38.3–52.9 Tg of C inorg , highlighting these meadows as hotspots for CaCO 3 burial. CaCO 3 contributes 67 ± 8% (mean ± standard error) of the sediment accumulation, indicating its important role in seabed elevation. Sediment C inorg showed no significant relationship with C org , with an average C org : C inorg ratio of 0.069 ± 0.002, ∼ 10 times lower than the threshold (C org : C inorg ratio of about 0.63) at which seagrass ecosystem transition from CO 2 sources to sinks. However, the available air–sea gas flux measurement was only 1/5 of the calculated CO 2 emission expected from calcification, suggesting that part of the accumulated CaCO 3 is supported by allochthonous inputs. Furthermore, no perceivable relationship between seagrass density and either CaCO 3 stock or accumulation rate was observed, indicating that seagrass may play a limited role in supporting CaCO 3 production. Further studies on water chemistry, calcification rate, air–sea CO 2 flux, and comparison between seagrass and unvegetated habitats are required to elucidate the carbon budget of this globally significant ecosystem

Biology · Blue carbon · Carbon dioxide · Carbon sequestration · Carbon sink · Carbonate · Ecosystem · Geography · Geomorphology · Seagrass · Sediment · Sink (geography · Total organic carbon · Chemistry · Coastal wetland ecosystem dynamics · Coral and Marine Ecosystems Studies · Environmental Science · Marine and coastal plant biology · Ecology · Geology · Oceanography

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