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Seasonal trends in the abundance, composition and bioavailability of particulate and dissolved organic matter in the Chukchi/Beaufort Seas and western Canada Basin

机译:楚科奇/波弗特海和加拿大西部海盆颗粒和溶解有机物的丰度,组成和生物利用度的季节性趋势

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The objectives of this study were to investigate the seasonality, abundance, sources and bioreactivity of organic matter in the water column of the western Arctic Ocean. The concentrations of particulate and dissolved amino acids and amino sugars, as well as bulk properties of particulate and dissolved organic matter (DOM), were measured in shelf, slope and basin waters collected during the spring and summer of 2002. Particulate organic matter concentrations in shelf waters increased by a factor of 10 between spring and summer. Dissolved organic carbon (DOC) and nitrogen (DON) concentrations exhibited only minor seasonal variations, whereas dissolved amino acid concentrations doubled between spring and summer, and dissolved amino sugars increased by 31% in shelf waters of the Chukchi and Beaufort Seas. Concentrations of DOC did not exhibit a significant seasonal change in surface waters of the Canada Basin, but dissolved amino acid concentrations increased by 45% between spring and summer. No significant seasonal differences were detected in the concentration or composition of DOM in waters below 100 m in depth. Concentrations of particulate and dissolved amino acids and amino sugars were strongly correlated with chlorophyll-a, indicating a plankton source of freshly produced organic matter. The amino acid and amino sugar compositions of freshly produced DOM indicated that a large portion of this material is bioavailable. While freshly produced DOM was found to be relatively bioreactive, preformed DOM in the Arctic appears to be less bioreactive but similar in degradation state to average DOM in the Atlantic and Pacific. These data demonstrate substantial summer production of POM and DOM on the Chukchi and Beaufort shelves that is available for utilization in shelf waters and export to the Canada Basin.
机译:这项研究的目的是调查北冰洋西部水柱中有机物的季节性,丰度,来源和生物反应性。在2002年春季和夏季收集的架子水,斜坡水和盆地水中,测量了颗粒和溶解的氨基酸和氨基糖的浓度,以及颗粒和溶解的有机物(DOM)的体积特性。在春季和夏季之间,架子水增加了10倍。在楚科奇海和博福特海的陆架水中,溶解的有机碳(DOC)和氮(DON)的浓度仅表现出较小的季节性变化,而溶解的氨基酸浓度在春季和夏季之间增加了一倍,并且溶解的氨基糖增加了31%。在加拿大盆地的地表水中,DOC的浓度没有显示出明显的季节性变化,但是在春季和夏季之间,溶解的氨基酸浓度增加了45%。在深度小于100 m的水中,DOM的浓度或组成没有发现明显的季节性差异。颗粒和溶解的氨基酸以及氨基糖的浓度与叶绿素-a密切相关,表明新鲜产生的有机物的浮游生物来源。新鲜生产的DOM的氨基酸和氨基糖成分表明该材料的很大一部分是可生物利用的。虽然发现新鲜产生的DOM具有相对生物活性,但北极中预制的DOM似乎生物活性较低,但降解状态与大西洋和太平洋地区的平均DOM相似。这些数据表明,楚科奇和博福特架子上夏季大量生产POM和DOM,可用于架子水域并出口到加拿大盆地。

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