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Seasonal and bleaching-induced changes in coral reef metabolism and CO2 flux

机译:季节性和漂白引起的珊瑚礁代谢和二氧化碳通量变化

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+AFs-1+AF0- Monitoring seawater CO2 for a full year with seasonal observations of community metabolism in Ishigaki Island, Japan, revealed seasonal variation and anomalous values owing to the bleaching event in 1998. The daily average pCO(2) showed a seasonal pattern on an annual scale, 280 to 320 mu atm in winter and 360 to 400 mu atm in summer, which was determined primarily by the seasonal change in seawater temperature. By contrast, the range in the diel variation in pCO(2), 400 to 500 mu atm in summer 200 to 300 matm in winter, was attributed to the seasonal variation in community metabolism: Gross primary production (P-g) and respiration ( R) were high in summer and low in winter. During the 1998 bleaching event, although Pg and R increased, community excess organic production ( E) decreased by three quarters compared with the same month in 1999, when the coral community showed high recovery. This change in metabolism led to large diel range and increased average value of pCO(2) levels in the seawater on the reef flat. The decrease in the range and increase in the average value of pCO(2) were observed by monitoring the Palau barrier reef flat, where overall mortality of corals occurred after the bleaching. All the metabolic parameters, Pg, R, E and calcification (G) were reduced by half after the bleaching, which increased the average pCO2 value by 10 matm and decreased its diel range from 200 - 400 mu atm to 100 - 200 mu atm. Bleaching and resultant mortality of coral reefs led to degradation of their metabolic performance, and thus resulted in the loss of their active interaction with the carbon cycle.
机译:+ AFs-1 + AF0-通过对日本石垣岛的社区代谢进行季节性观测,全年监测海水中的CO2,揭示了由于1998年的漂白事件造成的季节性变化和异常值。每日平均pCO(2)显示了季节性每年280-320大气压,夏季360-400大气压,这主要是由海水温度的季节性变化决定的。相比之下,pCO(2)diel变化的范围,夏季为400至500 mu atm,冬季为200至300 matm,归因于社区代谢的季节性变化:初级总生产(Pg)和呼吸(R)夏天高,冬天低。在1998年的漂白事件中,尽管Pg和R增加,但社区的有机过剩产量(E)与1999年同月相比下降了四分之三,当时珊瑚群落表现出很高的恢复能力。新陈代谢的这种变化导致大diel范围和礁滩上海水中pCO(2)水平的平均值增加。通过监测帕劳堡礁滩涂观察到了pCO(2)范围的减小和平均值的增加,那里的珊瑚总体死亡率在漂白后发生。漂白后所有代谢参数Pg,R,E和钙化(G)降低了一半,这使平均pCO2值增加了10 matm,并且diel范围从200-400微米大气压降低到100-200微米大气压。珊瑚礁的漂白和随之而来的死亡率导致其代谢性能下降,从而导致其与碳循环的主动相互作用丧失。

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