PHYTOPLANKTON CARBON TO CHLOROPHYLL "A" RATIO: RESPONSE TO LIGHT, TEMPERATURE AND NUTRIENT LIMITATION

Автор(и)

  • Z. Z. Finenko
  • N. Hoepffner
  • R. Williams
  • S. A. Piontkovski

Ключові слова:

углерод : хлорофилл а отношение, свет, температура, биогенное лимитирование, фотоадаптация, микроводоросли

Анотація

Выполнено обобщение литературных и собственных экспериментальных данных по действию света, температуры и биогенных элементов на отношение углерод-хлорофилл а в клетках 36 видов водорослей из 7 таксономических групп. При одинаковых условиях средние значения С:Хл. отношения для отдельных таксономических групп увеличиваются в следующем порядке: Chlorophyceae < Bacillariophyceae, Prochlorococcus < Prymnesiophyceae < Cyanophyceae < Dinophyceae. При постоянной температуре С:Хл. отношение повышается линейно с увеличением света и уменьшается экспоненциально с ростом температуры при одинаковой интенсивности света. Комбинированное действие света и температуры на С:Хл. отношение у всех исследованных водорослей описано одним уравнением с 3 коэффициентами. Согласно эмпирической модели, действие температуры на изменение С:Хл. отношения снижается с уменьшением интенсивности света. У всех таксономических групп водорослей при недостатке азота в среде С:Хл отношение увеличивается одинаковым образом при разных интенсивностях света. Создана модель, учитывающая комбинированное действие света, температуры и биогенных элементов на изменение С:Хл. отношения у микроводорослей. Располагая данными по распределению таксономического состава фитопланктона, концентрации биогенных элементов, ограничивающих скорость роста фитопланктона, температуры и интенсивности света на разных глубинах в олиго-, мезо- и эвтрофных водах тропической части Атлантического океана, по созданной модели рассчитаны С:Хл отношения в фитопланктоне, которые в верхнем перемешиваемом слое составили 145, 96 и 37 гС гХл а -1 соответственно, а у основания эвфотической зоны - 30 гС гХл а -1. Предложенная модель позволяет достаточно точно описать изменение отношения С:Хл у фитопланктона при различных условиях окружающей среды.

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2023-06-05