4.3 Article

Pattern and scale of variability among Northwest Atlantic Shelf plankton communities

期刊

JOURNAL OF PLANKTON RESEARCH
卷 32, 期 12, 页码 1661-1674

出版社

OXFORD UNIV PRESS
DOI: 10.1093/plankt/fbq058

关键词

zooplankton; phytoplankton; continuous plankton recorder; Gulf of Maine; Scotian Shelf; Middle Atlantic Bight; North Atlantic; climate variability

资金

  1. NSF [OCE-0625273]
  2. NERC [SAH01001] Funding Source: UKRI
  3. Natural Environment Research Council [SAH01001] Funding Source: researchfish

向作者/读者索取更多资源

Continuous plankton recorders (CPRs) have been used in the Northwest Atlantic for almost 50 years. While data collected by these surveys have provided valuable information on long-term variability in plankton populations, all previous analyses have been limited to only a portion of the geographic range of the available data. Here we present an analysis of the CPR data from the Mid Atlantic Bight to the Labrador Sea. Across this wide geographic range, we found many common associations among the taxa. In particular, the changes in most regions were strongly size structured, with small and medium copepods varying together and often positively related to indicators of phytoplankton abundance. The time series from nearby regions were strongly correlated; however, after 1990, the spatial pattern became more complex. During this period, several of the copepod taxa, noticeably Calanus finmarchicus and Centropages typicus, experienced a series of anomalies that appeared to propagate from northeast to southwest. Although the direction of propagation was consistent with the shelf circulation, the anomalies propagated at a rate much slower than typical current speeds. The timing of the copepod anomalies and their phase speed were similar in character to observed changes in salinity and the position of the Shelf Slope Front. The correspondence between the changes in the plankton community and changes in the physical environmental suggests that physical conditions are a strong driver of interannual variability in Northwest Atlantic Shelf ecosystems.

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