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Carbon and nitrogen cycling in the Zhubi coral reef lagoon of the South China Sea as revealed by 210Po and 210Pb

► 210Po/210Pb disequilibria were used to trace export of POC and PON in a coral lagoon. ► Recycling of POC and PON were quantified by a mass balance budget in a coral lagoon. ► 210Po excess could be used to qualify the degradation of particulate organic matter. ► Degradation rate constant of POM was...

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Published in:Marine pollution bulletin 2011-05, Vol.62 (5), p.905-911
Main Authors: Yang, W.F., Huang, Y.P., Chen, M., Qiu, Y.S., Li, H.B., Zhang, L.
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cited_by cdi_FETCH-LOGICAL-c404t-99e68fcd7a9ea7c69cee7eb6faff821f3af65b21feda63e147c39066e260078f3
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description ► 210Po/210Pb disequilibria were used to trace export of POC and PON in a coral lagoon. ► Recycling of POC and PON were quantified by a mass balance budget in a coral lagoon. ► 210Po excess could be used to qualify the degradation of particulate organic matter. ► Degradation rate constant of POM was much more in the lagoon than in the open sea. The radionuclides 210Po and 210Pb were examined to trace the cycling of particulate organic carbon (POC) and particulate organic nitrogen (PON) in the Zhubi coral reef lagoon. The net export flux of POC to the open sea is 14mgCm−2d−1. However, the net exchange of PON has not yet been observed. On average, the vertical export fluxes in the lagoon of POC and PON, as derived from 210Po/210Pb disequilibria, are 43mgCm−2d−1 and 13.8mgNm−2d−1, respectively. The deficit of 210Po relative to 210Pb in particulate matter provides evidence for the degradation of particulate organic matter. According to the mass balance budgets, 310mgCm−2d−1 and 121mgNm−2d−1 were recycled into dissolved fractions. Based on a first-order kinetics model, the degradation rate constants of POC and PON are 0.28 and 0.30m−1, respectively. Thus, 210Po and 210Pb can quantify the cycling of carbon and nitrogen in this coral lagoon.
doi_str_mv 10.1016/j.marpolbul.2011.02.058
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The radionuclides 210Po and 210Pb were examined to trace the cycling of particulate organic carbon (POC) and particulate organic nitrogen (PON) in the Zhubi coral reef lagoon. The net export flux of POC to the open sea is 14mgCm−2d−1. However, the net exchange of PON has not yet been observed. On average, the vertical export fluxes in the lagoon of POC and PON, as derived from 210Po/210Pb disequilibria, are 43mgCm−2d−1 and 13.8mgNm−2d−1, respectively. The deficit of 210Po relative to 210Pb in particulate matter provides evidence for the degradation of particulate organic matter. According to the mass balance budgets, 310mgCm−2d−1 and 121mgNm−2d−1 were recycled into dissolved fractions. Based on a first-order kinetics model, the degradation rate constants of POC and PON are 0.28 and 0.30m−1, respectively. 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Psychology ; International trade ; Lagoons ; lead ; Lead Radioisotopes - analysis ; Marine ; nitrogen ; Nitrogen - analysis ; Nitrogen Cycle ; Oceans and Seas ; organic matter ; particulates ; POC ; Polonium - analysis ; Radioactive Tracers ; radionuclides ; Recycled ; recycling ; Sea water ecosystems ; Seawater - chemistry ; South China Sea ; Synecology ; Water Pollutants, Chemical - analysis ; water pollution</subject><ispartof>Marine pollution bulletin, 2011-05, Vol.62 (5), p.905-911</ispartof><rights>2011 Elsevier Ltd</rights><rights>2015 INIST-CNRS</rights><rights>Copyright © 2011 Elsevier Ltd. 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The radionuclides 210Po and 210Pb were examined to trace the cycling of particulate organic carbon (POC) and particulate organic nitrogen (PON) in the Zhubi coral reef lagoon. The net export flux of POC to the open sea is 14mgCm−2d−1. However, the net exchange of PON has not yet been observed. On average, the vertical export fluxes in the lagoon of POC and PON, as derived from 210Po/210Pb disequilibria, are 43mgCm−2d−1 and 13.8mgNm−2d−1, respectively. The deficit of 210Po relative to 210Pb in particulate matter provides evidence for the degradation of particulate organic matter. According to the mass balance budgets, 310mgCm−2d−1 and 121mgNm−2d−1 were recycled into dissolved fractions. Based on a first-order kinetics model, the degradation rate constants of POC and PON are 0.28 and 0.30m−1, respectively. 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The radionuclides 210Po and 210Pb were examined to trace the cycling of particulate organic carbon (POC) and particulate organic nitrogen (PON) in the Zhubi coral reef lagoon. The net export flux of POC to the open sea is 14mgCm−2d−1. However, the net exchange of PON has not yet been observed. On average, the vertical export fluxes in the lagoon of POC and PON, as derived from 210Po/210Pb disequilibria, are 43mgCm−2d−1 and 13.8mgNm−2d−1, respectively. The deficit of 210Po relative to 210Pb in particulate matter provides evidence for the degradation of particulate organic matter. According to the mass balance budgets, 310mgCm−2d−1 and 121mgNm−2d−1 were recycled into dissolved fractions. Based on a first-order kinetics model, the degradation rate constants of POC and PON are 0.28 and 0.30m−1, respectively. Thus, 210Po and 210Pb can quantify the cycling of carbon and nitrogen in this coral lagoon.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><pmid>21450313</pmid><doi>10.1016/j.marpolbul.2011.02.058</doi><tpages>7</tpages></addata></record>
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ispartof Marine pollution bulletin, 2011-05, Vol.62 (5), p.905-911
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1879-3363
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source ScienceDirect Freedom Collection 2022-2024
subjects 210Pb
210Po
Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
Carbon
Carbon - analysis
Carbon Cycle
China
Coral reef lagoon
Coral Reefs
corals
Cycles
Degradation
Environmental Monitoring - methods
Exports
Fundamental and applied biological sciences. Psychology
International trade
Lagoons
lead
Lead Radioisotopes - analysis
Marine
nitrogen
Nitrogen - analysis
Nitrogen Cycle
Oceans and Seas
organic matter
particulates
POC
Polonium - analysis
Radioactive Tracers
radionuclides
Recycled
recycling
Sea water ecosystems
Seawater - chemistry
South China Sea
Synecology
Water Pollutants, Chemical - analysis
water pollution
title Carbon and nitrogen cycling in the Zhubi coral reef lagoon of the South China Sea as revealed by 210Po and 210Pb
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