A Regional, Early Spring Bloom of Phaeocystis pouchetii on the New England Continental Shelf
A Regional, Early Spring Bloom of Phaeocystis pouchetii on the New England Continental Shelf
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DOI:
10.1029/2020jc016856
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发表时间:
2021-02
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通讯作者:
W. Smith;W. Zhang;Andrew J. Hirzel;R. Stanley;M. G. Meyer;H. Sosik;P. Alatalo;H. Oliver;Z. Sandwith;E. T. Crockford;Emily E. Peacock;Arshi Mehta;D. McGillicuddy
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作者:
W. Smith;W. Zhang;Andrew J. Hirzel;R. Stanley;M. G. Meyer;H. Sosik;P. Alatalo;H. Oliver;Z. Sandwith;E. T. Crockford;Emily E. Peacock;Arshi Mehta;D. McGillicuddy
The genus Phaeocystis is distributed globally throughout the world's oceans, forming blooms in European, Asian, Antarctic, Arctic, and North American waters and in tropical, polar and temperate systems. It often (but not always) releases dimethylsulfide into the surface layer, which has the potential for altering weather and climate patterns (Charlson et al., 1987; Stefels et al., 1995), and significantly influences the biogeochemistry of sulfur (Wang et al., 2016). In addition, Phaeocystis is considered to be largely “unpalatable” to zooplankton grazers (Nejstgaard et al., 2007). The ecology and physiology of Phaeocystis are relatively well studied, but given the variety of environments the genus can occupy, it is difficult to generalize about Abstract The genus Phaeocystis is distributed globally and has considerable ecological, biogeochemical, and societal impacts. Understanding its distribution, growth and ecological impacts has been limited by lack of extensive observations on appropriate scales. In 2018, we investigated the biological dynamics of the New England continental shelf and encountered a substantial bloom of Phaeocystis pouchetii. Based on satellite imagery during January through April, the bloom extended over broad expanses of the shelf; furthermore, our observations demonstrated that it reached high biomass levels, with maximum chlorophyll concentrations exceeding 16 μg L and particulate organic carbon levels > 95 μmol L. Initially, the bloom was largely confined to waters with temperatures <6°C, which in turn were mostly restricted to shallow areas near the coast. As the bloom progressed, it appeared to sink into the bottom boundary layer; however, enough light and nutrients were available for growth. The bloom was highly productive (net community production integrated through the mixed layer from stations within the bloom averaged 1.16 g C m d) and reduced nutrient concentrations considerably. Long-term coastal observations suggest that Phaeocystis blooms occur sporadically in spring on Nantucket Shoals and presumably expand onto the continental shelf. Based on the distribution of Phaeocystis during our study, we suggest that it can have a significant impact on the overall productivity and ecology of the New England shelf during the winter/spring transition.