4.6 Review

Basin-scale variability in phytoplankton size-abundance spectra across the Atlantic Ocean

期刊

PROGRESS IN OCEANOGRAPHY
卷 217, 期 -, 页码 -

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.pocean.2023.103104

关键词

-

向作者/读者索取更多资源

Phytoplankton size structure, as indicated by the slope of the size-abundance spectrum, plays a vital role in determining trophic structure and functioning in pelagic ecosystems. Previous studies have primarily focused on specific open-ocean or coastal environments, thus neglecting the overall variability in phytoplankton size structure across wide ranges of biomass and productivity. In this study, we provide a comprehensive overview of the basin-scale variability in phytoplankton biomass and size-abundance spectrum slope across the Atlantic Ocean, revealing consistent latitudinal patterns and an inverse relationship between cell size and abundance. These findings have implications for understanding and predicting shifts in phytoplankton size structure in response to climate change.
Phytoplankton size structure, a major determinant of trophic structure and biogeochemical functioning in pelagic ecosystems, can be described by the slope of the size-abundance spectrum (SAS). Previous observational studies reporting spatio-temporal changes in phytoplankton SAS slope have focused on particular open-ocean or coastal environments. Therefore, the overall variability in phytoplankton SAS slope still has not been investigated over wide ranges of biomass and productivity including both oligotrophic open-ocean regions and productive coastal waters. Here we present a multi-cruise overview of the basin-scale variability in phytoplankton biomass and SAS slope across the Atlantic Ocean, covering coastal, shelf, and oceanic environments over the 50 degrees N-50 degrees S latitude range. We find the inverse relationship between cell size and abundance to be pervasive across the studied regions, even in highly productive coastal waters. In oceanic regions, consistent latitudinal patterns are observed in the relationship between nutricline depth, phytoplankton biomass and SAS slope. There is a strong degree of covariation between SAS slope at the surface and at the base of the euphotic layer, indicating that geographical changes in phytoplankton size structure override vertical variability. A basin-scale relationship exists between increasing resource supply, enhanced phytoplankton biomass, and progressively less steep SAS slopes, reflecting increasing importance of large cells in more productive waters. However, the relationship between ecosystem productivity and both SAS slope and mean community cell size is saturating, which means there is no continuous trend towards ever increasing contribution by larger cells. Similar phytoplankton size structures, with a biomass dominance by the 2-20 & mu;m size class, are found in both moderately and highly eutrophic waters. Our results provide an observational benchmark for testing the predictions of size-based plankton models and for assessing future, climate-related shifts in phytoplankton size structure in both coastal and oceanic regions of the Atlantic Ocean.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.6
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据