TY - JOUR
T1 - Sargassum sp. Act as a Large Regional Source of Marine Dissolved Organic Carbon and Polyphenols
AU - Powers, Leanne C.
AU - Hertkorn, Norbert
AU - McDonald, Natasha
AU - Schmitt-Kopplin, Philippe
AU - Del Vecchio, Rossana
AU - Blough, Neil V.
AU - Gonsior, Michael
N1 - Publisher Copyright:
© 2019. American Geophysical Union. All Rights Reserved.
PY - 2019/11/1
Y1 - 2019/11/1
N2 - Dissolved organic carbon (DOC) plays critical roles in marine carbon cycling, but its sources and sinks remain uncertain. In this study, we monitored DOC exudation rates of Sargassum natans under visible light (λ > 390 nm) and solar radiation. DOC release rates ranged from 7 to 10 μg C g−1 biomass hr−1 (wet weight) under visible light, but increased to 23 to 41 μg C g−1 biomass hr−1 when exposed to natural sunlight. Results indicate that DOC released by Sargassum could amount to 0.3 to 1.2 Tg C/year, potentially contributing significantly to the marine DOC pool in the Gulf of Mexico and Western North Atlantic. We employed the Folin-Ciocalteu phenolic content method, nuclear magnetic resonance (NMR) spectroscopy, and ultrahigh resolution Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) to characterize the diverse pool of organic compounds exuded from Sargassum. Results from these complementary methods showed that Sargassum release large quantities of phlorotannins, a class of polyphenols that have very similar properties to terrestrial DOC. These phlorotannins and their oxygenated phenolic derivatives exhibit a high hydrogen deficiency and functionalization (i.e., 4 to 6 oxygen atoms per aromatic ring), representing 5 to 18% of the released DOC isolated by solid phase extraction. Thus, Sargassum is the largest biological source of open ocean polyphenols recorded to date. The amount of polyphenolic DOC released by Sargassum challenges previous beliefs that all polyphenols found within the oceans are remnants of terrestrial organic matter, although the stability of phlorotannins and their derivatives needs to be further evaluated.
AB - Dissolved organic carbon (DOC) plays critical roles in marine carbon cycling, but its sources and sinks remain uncertain. In this study, we monitored DOC exudation rates of Sargassum natans under visible light (λ > 390 nm) and solar radiation. DOC release rates ranged from 7 to 10 μg C g−1 biomass hr−1 (wet weight) under visible light, but increased to 23 to 41 μg C g−1 biomass hr−1 when exposed to natural sunlight. Results indicate that DOC released by Sargassum could amount to 0.3 to 1.2 Tg C/year, potentially contributing significantly to the marine DOC pool in the Gulf of Mexico and Western North Atlantic. We employed the Folin-Ciocalteu phenolic content method, nuclear magnetic resonance (NMR) spectroscopy, and ultrahigh resolution Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) to characterize the diverse pool of organic compounds exuded from Sargassum. Results from these complementary methods showed that Sargassum release large quantities of phlorotannins, a class of polyphenols that have very similar properties to terrestrial DOC. These phlorotannins and their oxygenated phenolic derivatives exhibit a high hydrogen deficiency and functionalization (i.e., 4 to 6 oxygen atoms per aromatic ring), representing 5 to 18% of the released DOC isolated by solid phase extraction. Thus, Sargassum is the largest biological source of open ocean polyphenols recorded to date. The amount of polyphenolic DOC released by Sargassum challenges previous beliefs that all polyphenols found within the oceans are remnants of terrestrial organic matter, although the stability of phlorotannins and their derivatives needs to be further evaluated.
KW - DOC
KW - FT-ICR MS
KW - NMR
KW - Sargassum
KW - marine dissolved organic matter
KW - marine polyphenols
UR - http://www.scopus.com/inward/record.url?scp=85075586062&partnerID=8YFLogxK
U2 - 10.1029/2019GB006225
DO - 10.1029/2019GB006225
M3 - Article
AN - SCOPUS:85075586062
SN - 0886-6236
VL - 33
SP - 1423
EP - 1439
JO - Global Biogeochemical Cycles
JF - Global Biogeochemical Cycles
IS - 11
ER -