Bio-optical evidence for increasing Phaeocystis dominance in the Barents Sea

被引:29
|
作者
Orkney, A. [1 ]
Platt, T. [2 ]
Narayanaswamy, B. E. [3 ]
Kostakis, I [4 ,5 ]
Bouman, H. A. [1 ]
机构
[1] Univ Oxford, Dept Earth Sci, 3 South Parks Rd, Oxford OX1 3AN, England
[2] Plymouth Marine Lab, Prospect Pl, Plymouth PL1 3DH, Devon, England
[3] Scottish Marine Inst, Scottish Assoc Marine Sci, Oban PA37 1QA, Argyll, Scotland
[4] Univ Portsmouth, Sch Comp, Portsmouth PO1 3HE, Hants, England
[5] Univ Strathclyde, Phys Dept, Glasgow G4 0NG, Lanark, Scotland
基金
英国自然环境研究理事会;
关键词
phaeocystis; Arctic; phytoplankton; climate; ocean-colour; remote-sensing; MARGINAL ICE-ZONE; BLOOMS; EXPORT; PRYMNESIOPHYCEAE; SEDIMENTATION; VARIABILITY; DIATOMS; IMPACT; WATERS;
D O I
10.1098/rsta.2019.0357
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Increasing contributions of prymnesiophytes such as Phaeocystis pouchetii and Emiliania huxleyi to Barents Sea (BS) phytoplankton production have been suggested based on in situ observations of phytoplankton community composition, but the scattered and discontinuous nature of these records confounds simple inference of community change or its relationship to salient environmental variables. However, provided that meaningful assessments of phytoplankton community composition can be inferred based on their optical characteristics, ocean-colour records offer a potential means to develop a synthesis between sporadic in situ observations. Existing remote-sensing algorithms to retrieve phytoplankton functional types based on chlorophyll-a (chl-a) concentration or indices of pigment packaging may, however, fail to distinguish Phaeocystis from other blooms of phytoplankton with high pigment packaging, such as diatoms. We develop a novel algorithm to distinguish major phytoplankton functional types in the BS and apply it to the MODIS-Aqua ocean-colour record, to study changes in the composition of BS phytoplankton blooms in July, between 2002 and 2018, creating time series of the spatial distribution and intensity of coccolithophore, diatom and Phaeocystis blooms. We confirm a north-eastward expansion in coccolithophore bloom distribution, identified in previous studies, and suggest an inferred increase in chl-a concentrations, reported by previous researchers, may be partly explained by increasing frequencies of Phaeocystis blooms. This article is part of the theme issue 'The changing Arctic Ocean: consequences for biological communities, biogeochemical processes and ecosystem functioning'.
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页数:16
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