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Seasonal dynamics and net production of dissolved organic carbon in an oligotrophic coastal environment

机译:贫营养海岸环境中溶解有机碳的季节动态和净产量

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摘要

To understand dissolved organic carbon (DOC) seasonal dynamics in a coastal oligotrophic site in the north-western Mediterranean Sea, we monitored DOC concentrations monthly over 3 yr, together with the meteorological data and the food-web-related biological processes involved in DOC dynamics. Additional DOC samples were taken in several inshore-offshore transects along the Catalan coast. We found DOC concentrations of ~60 μmol C 1~(-1) in winter, with increasing values through the summer and autumn and reaching 100 to 120 μmol C 1~(-1) in November. There was high inter-annual variability in this summer DOC accumulation, with values of 36, 69 and 13 umol C 1~(-1) for 2006, 2007 and 2008, respectively. The analysis of the microbial food-web processes involved in the DOC balance did not reveal the causes of this accumulation, since the only occasion on which we observed net DOC production (0.3 ± 1 umol C 1~(-1) d~(-1) on average) was in 2007, and the negative DOC balance of 2006 and 2008 did not prevent DOC accumulating. The DOC accumulation episodes coincided with low rates of water renewal (average 0.037 ± 0.021 d~(-1) from May to October) compared with those of winter to early spring (average 0.11 ± 0.048 d~(-1) from November to April). Indeed, the amount of DOC accumulated each year was inversely correlated with the average summer rainfall. We hypothesize that decreased DOC turn-over due to photochemical or biological processes-mostly active during the summer-and low water renewal rate combine to determine seasonal DOC accumulation and influence its inter-annual variability.
机译:为了了解西北地中海沿岸贫营养化站点中溶解有机碳(DOC)的季节动态,我们在3年中每月监测DOC浓度,以及气象数据和与DOC动态有关的与食物网相关的生物过程。在加泰罗尼亚海岸的几个近海-近海样带中采集了额外的DOC样本。我们发现冬季的DOC浓度为〜60μmolC 1〜(-1),在夏季和秋季均呈上升趋势,11月达到100至120μmolC 1〜(-1)。夏季DOC的年际变化较大,2006、2007和2008年的值分别为36、69和13 umol C 1〜(-1)。对DOC平衡中涉及的微生物食物网过程的分析并未揭示这种积累的原因,因为我们唯一观察到的是DOC净产量(0.3±1 umol C 1〜(-1)d〜(- 1)的平均值是2007年,而2006和2008年的DOC负余额并未阻止DOC的累积。与冬季至早春(11月至4月的平均值为0.11±0.048 d〜(-1))相比,DOC累积事件与低水质更新率(5月至10月的平均值为0.037±0.021 d〜(-1))一致。 )。确实,每年积累的DOC量与夏季平均降雨量成反比。我们假设由于光化学或生物过程而导致的DOC周转量减少(通常在夏季活跃)和较低的水更新率共同决定了季节性DOC的积累并影响其年际变化。

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