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The Evolution of Modern Eukaryotic Phytoplankton

2004· review· en· 1,587 citations· W2136668140 on OpenAlex· 10.1126/science.1095964

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Canadian affiliationAn author listed a Canadian institution. This is the only route the usual frame has.

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Opus teacher head0.026
GPT teacher head0.273
Teacher spread
0.246 · how far apart the two teachers sit on this one work
Validation status
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Abstract

The community structure and ecological function of contemporary marine ecosystems are critically dependent on eukaryotic phytoplankton. Although numerically inferior to cyanobacteria, these organisms are responsible for the majority of the flux of organic matter to higher trophic levels and the ocean interior. Photosynthetic eukaryotes evolved more than 1.5 billion years ago in the Proterozoic oceans. However, it was not until the Mesozoic Era (251 to 65 million years ago) that the three principal phytoplankton clades that would come to dominate the modern seas rose to ecological prominence. In contrast to their pioneering predecessors, the dinoflagellates, coccolithophores, and diatoms all contain plastids derived from an ancestral red alga by secondary symbiosis. Here we examine the geological, geochemical, and biological processes that contributed to the rise of these three, distantly related, phytoplankton groups.

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The record

Venue
Science
Topic
Paleontology and Stratigraphy of Fossils
Field
Earth and Planetary Sciences
Canadian institutions
University of British Columbia
Funders
Keywords
PhytoplanktonEcologyEcosystemTrophic levelMarine ecosystemOceanographyBiologyMesozoicPlastidPrimary producersProterozoicPaleontologyGeologyStructural basinNutrientChloroplast
Has abstract in OpenAlex
yes