4.4 Article

Distribution of Sprattus sprattus phalericus (Risso, 1827) and zooplankton near the Black Sea redoxcline

期刊

JOURNAL OF FISH BIOLOGY
卷 99, 期 4, 页码 1393-1402

出版社

WILEY
DOI: 10.1111/jfb.14848

关键词

feeding hypoxiaSprattus sprattus phalericus suboxic zone zooplankton

资金

  1. German Research Foundation [01DK12043]
  2. Russian Academy of Science [AAAA-A18-118020790229-7]
  3. russian academy of sciences (ru) [AAAA-A18-118021490093-4]
  4. Russian Academy of Sciences

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Understanding the environmental drivers of marine predator-prey relationships is crucial for ecosystem management, especially in environments like the Black Sea. Research in the north-eastern Black Sea showed that Black Sea sprat can tolerate hypoxic waters near the redoxcline, with some individuals descending to deeper layers for foraging. Zooplankton were observed concentrated on the upper boundary of the suboxic zone, with none observed below certain oxygen concentrations. Understanding the tolerance of this species to low oxygen conditions is important for predicting its responses to future changes in hypoxia.
Understanding what environmental drivers influence marine predator-prey relationships can be key to managing and protecting ecosystems, especially in the face of future climate change risks. This is especially important in environments such as the Black Sea, where strong biogeochemical gradients can drive marine habitat partitioning and ecological interactions. We used underwater video recordings in the north-eastern Black Sea in November 2013 to observe the distribution and behaviour of the Black Sea sprat (Sprattus sprattus phalericus, Risso 1827) and its zooplankton prey. Video recordings have shown that the Black Sea sprat S. sprattus phalericus tolerates severely hypoxic waters near the redoxcline. The school was distributed in the 33-96 m layer [oxygen concentration (O-2) 277-84 mu mol L-1]. Some individuals were observed to leave the school and descended 20 m deeper for foraging on copepods in the 119-123 m layer (O-2 12-10 mu mol L-1). Zooplankton appeared concentrated on the upper boundary of the suboxic zone (O-2 < 10 mu mol L-1). No zooplankton were observed below O-2 6-7 mu mol L-1 (128 m). Understanding the ability of this species to tolerate low oxygen waters is crucial to predicting future responses to natural and anthropogenic changes in hypoxia.

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