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DISTRIBUTIONS OF FREE AMINO ACIDS IN SEA AND LAKE ICE CORES FROM ANTARCTICA WITH SPECIAL REFERENCE TO ICE BIOTA (16th Symposium on Polar Biology)

机译:南极海冰和冰核中游离氨基酸的分布特别参考冰生物学(第16届极地生物学研讨会)

摘要

Dissolved free amino acids (DFAA) of sea ice cores and lake ice cores collected from the vicinity of Davis Station, Antarctica were determined by HPLC. The results of DFAA analysis showed that concentrations of total DFAA in ice cores were higher compared to those in water and they varied from 8.0 μM to 30.9μM and 14.0 μM to 45.0 μM in the sea and lake ice cores, respectively. The highest concentration of total DFAA in the sea ice core appeared in the bottom of 150cm depth, while that in the lake ice core was found in the middle part of the 60-70 cm depth. The relative compositions of individual amino acids, such as serine, histidine and ornithine, which were present in higher concentrations, were similar in both types of ice cores. The variation in the total concentration of DFAA was related to the variation in microalgal cell numbers in the sea ice cores. These DFAA were probably derived from metabolism of the dominant organisms in the algal assemblage ice community. These amino acids are stored in the ice as a large portion of the dissolved organic matter (DOM). It is assumed that these amino acids might be a source of carbon and nitrogen for phytoplankton and/or other microorganisms which bloom during (the next) summer season in the water column.
机译:通过HPLC测定从南极州戴维斯站附近收集的海冰芯和湖冰芯的溶解游离氨基酸(DFAA)。 DFAA分析的结果表明,冰芯中的总DFAA浓度比水中的高,并且在海冰芯和湖冰芯中,它们的浓度分别为8.0μM至30.9μM和14.0μM至45.0μM。海冰芯中总DFAA的最高浓度出现在150cm深度的底部,而湖冰芯中的最高DFAA浓度则出现在60-70 cm深度的中部。在两种类型的冰芯中,浓度较高的单个氨基酸(如丝氨酸,组氨酸和鸟氨酸)的相对组成相似。 DFAA总浓度的变化与海冰芯中微藻细胞数量的变化有关。这些DFAA可能源自藻类组合冰群落中优势生物的代谢。这些氨基酸以大部分溶解有机物(DOM)的形式存储在冰中。假定这些氨基酸可能是浮游植物和/或在(下一)夏季在水柱中开花的浮游植物和/或其他微生物的碳和氮的来源。

著录项

  • 作者

    Hefu YANG;

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  • 年度 1995
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  • 原文格式 PDF
  • 正文语种 en
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