Source, distribution, and transformation of dissolved and particulate organic matters in Qinzhou Bay, Northern Beibu Gulf

Both dissolved and particulate organic matters (DOM and POM) provide a reduced carbon pool of considerable size in coastal ecosystems, and the two are closely linked. Currently, however, the integrated study of DOM and POM remains limited, precluding a more in-depth understanding of their interactio...

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Main Authors: Shangjun Cai, Chao Wang, Qingmei Zhu, Qibin Lao
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-04-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2023.1163899/full
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author Shangjun Cai
Chao Wang
Chao Wang
Chao Wang
Chao Wang
Qingmei Zhu
Qingmei Zhu
Qingmei Zhu
Qibin Lao
author_facet Shangjun Cai
Chao Wang
Chao Wang
Chao Wang
Chao Wang
Qingmei Zhu
Qingmei Zhu
Qingmei Zhu
Qibin Lao
author_sort Shangjun Cai
collection DOAJ
description Both dissolved and particulate organic matters (DOM and POM) provide a reduced carbon pool of considerable size in coastal ecosystems, and the two are closely linked. Currently, however, the integrated study of DOM and POM remains limited, precluding a more in-depth understanding of their interaction in coastal regions. In April 2021, 13 surface water samples were collected from Qinzhou Bay, in the northern Beibu Gulf. The DOM samples were characterized using dissolved organic carbon (DOC) analysis and UV-visible and fluorescence spectroscopy techniques. We determined the POM for the particulate organic carbon and nitrogen (POC and PN) and also isotopic composition (δ13C and δ15N). The weak to negligible relationships found between the DOC, colored and fluorescent DOM, salinity, and chlorophyll a together suggested that DOM’s distribution in Qinzhou Bay is concurrently shaped by various processes, namely, hydrological and in situ biological processes. A high C/N ratio of ~17, high POC/chlorophyll a ratio (253 ± 112), and depleted δ13C (−25.7 ± 1.6‰) confirmed that POM is highly degraded and originates mainly from allochthonous input, to which the terrigenous organic matter and freshwater phytoplankton each contributes 35%. The total organic carbon (TOC = DOC + POC) was positively correlated with the humic-like peak M, revealing the transformation of labile DOM and POM into recalcitrant DOM components. The in situ production efficiency of peak M in surface waters of Qinzhou Bay is one order of magnitude greater than that in inland waters or open oceans, indicating that not only temperature but also the activity of substrate is a key factor controlling the in situ production of recalcitrant DOM in Qinzhou Bay. High levels of TOC and humic-like fluorescent DOM suggest the mass coexistence of organic matter differing in its reactivity, highlighting the large potential for photochemical as well as microbial degradation in the future.
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spelling doaj.art-bc382a6e9bb748bebfcd5755948cef0c2023-04-18T05:18:49ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452023-04-011010.3389/fmars.2023.11638991163899Source, distribution, and transformation of dissolved and particulate organic matters in Qinzhou Bay, Northern Beibu GulfShangjun Cai0Chao Wang1Chao Wang2Chao Wang3Chao Wang4Qingmei Zhu5Qingmei Zhu6Qingmei Zhu7Qibin Lao8College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, ChinaCollege of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, ChinaLaboratory for Coastal Ocean Variation and Disaster Prediction, College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, ChinaKey Laboratory of Climate, Resources and Environment in Continental Shelf Sea and Deep Sea of Department of Education of Guangdong Province, Guangdong Ocean University, Zhanjiang, ChinaKey Laboratory of Space Ocean Remote Sensing and Application, Ministry of Natural Resources, Beijing, ChinaCollege of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, ChinaLaboratory for Coastal Ocean Variation and Disaster Prediction, College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, ChinaKey Laboratory of Climate, Resources and Environment in Continental Shelf Sea and Deep Sea of Department of Education of Guangdong Province, Guangdong Ocean University, Zhanjiang, ChinaCollege of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, ChinaBoth dissolved and particulate organic matters (DOM and POM) provide a reduced carbon pool of considerable size in coastal ecosystems, and the two are closely linked. Currently, however, the integrated study of DOM and POM remains limited, precluding a more in-depth understanding of their interaction in coastal regions. In April 2021, 13 surface water samples were collected from Qinzhou Bay, in the northern Beibu Gulf. The DOM samples were characterized using dissolved organic carbon (DOC) analysis and UV-visible and fluorescence spectroscopy techniques. We determined the POM for the particulate organic carbon and nitrogen (POC and PN) and also isotopic composition (δ13C and δ15N). The weak to negligible relationships found between the DOC, colored and fluorescent DOM, salinity, and chlorophyll a together suggested that DOM’s distribution in Qinzhou Bay is concurrently shaped by various processes, namely, hydrological and in situ biological processes. A high C/N ratio of ~17, high POC/chlorophyll a ratio (253 ± 112), and depleted δ13C (−25.7 ± 1.6‰) confirmed that POM is highly degraded and originates mainly from allochthonous input, to which the terrigenous organic matter and freshwater phytoplankton each contributes 35%. The total organic carbon (TOC = DOC + POC) was positively correlated with the humic-like peak M, revealing the transformation of labile DOM and POM into recalcitrant DOM components. The in situ production efficiency of peak M in surface waters of Qinzhou Bay is one order of magnitude greater than that in inland waters or open oceans, indicating that not only temperature but also the activity of substrate is a key factor controlling the in situ production of recalcitrant DOM in Qinzhou Bay. High levels of TOC and humic-like fluorescent DOM suggest the mass coexistence of organic matter differing in its reactivity, highlighting the large potential for photochemical as well as microbial degradation in the future.https://www.frontiersin.org/articles/10.3389/fmars.2023.1163899/fullQinzhou bayBeibu Gulfdissolved organic matterparticulate organic matterabsorption and fluorescence spectraδ13C and δ15N
spellingShingle Shangjun Cai
Chao Wang
Chao Wang
Chao Wang
Chao Wang
Qingmei Zhu
Qingmei Zhu
Qingmei Zhu
Qibin Lao
Source, distribution, and transformation of dissolved and particulate organic matters in Qinzhou Bay, Northern Beibu Gulf
Frontiers in Marine Science
Qinzhou bay
Beibu Gulf
dissolved organic matter
particulate organic matter
absorption and fluorescence spectra
δ13C and δ15N
title Source, distribution, and transformation of dissolved and particulate organic matters in Qinzhou Bay, Northern Beibu Gulf
title_full Source, distribution, and transformation of dissolved and particulate organic matters in Qinzhou Bay, Northern Beibu Gulf
title_fullStr Source, distribution, and transformation of dissolved and particulate organic matters in Qinzhou Bay, Northern Beibu Gulf
title_full_unstemmed Source, distribution, and transformation of dissolved and particulate organic matters in Qinzhou Bay, Northern Beibu Gulf
title_short Source, distribution, and transformation of dissolved and particulate organic matters in Qinzhou Bay, Northern Beibu Gulf
title_sort source distribution and transformation of dissolved and particulate organic matters in qinzhou bay northern beibu gulf
topic Qinzhou bay
Beibu Gulf
dissolved organic matter
particulate organic matter
absorption and fluorescence spectra
δ13C and δ15N
url https://www.frontiersin.org/articles/10.3389/fmars.2023.1163899/full
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