ArticleScience advances2021
Truncated bimodal latitudinal diversity gradient in early Paleozoic phytoplankton.
Article in Science advances, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 8 papers.
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Who cites it
8 citing papers in PubMed.
- Unravelling the drivers of marine biodiversity across the Phanerozoic.Nature communications · 2025Article
- A niche-based theory of island biogeography.Ecology and evolution · 2024Article
- Colonial green algae in the Cambrian plankton.Proceedings. Biological sciences · 2023Article
- Impact of global climate cooling on Ordovician marine biodiversity.Nature communications · 2023Article
- Occurrence-based diversity estimation reveals macroecological and conservation knowledge gaps for global woody plants.Science advances · 2023Article
- Why the Early Paleozoic was intrinsically prone to marine extinction.Science advances · 2023Article
- Review
- Palaeoecology of Cambrian-Ordovician acritarchs from China: evidence for a progressive invasion of the marine habitats.Philosophical transactions of the Royal Society of London. Series B, Biological sciences · 2022Article
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Authors and funding
7 authors.
Funding
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Abstract
The latitudinal diversity gradient (LDG)-the decline in species richness from the equator to the poles-is classically considered as the most pervasive macroecological pattern on Earth, but the timing of its establishment, its ubiquity in the geological past, and explanatory mechanisms remain uncertain. By combining empirical and modeling approaches, we show that the first representatives of marine phytoplankton exhibited an LDG from the beginning of the Cambrian, when most major phyla appeared. However, this LDG showed a single peak of diversity centered on the Southern Hemisphere, in contrast to the equatorial peak classically observed for most modern taxa. We find that this LDG most likely corresponds to a truncated bimodal gradient, which probably results from an uneven sediment preservation, smaller sampling effort, and/or lower initial diversity in the Northern Hemisphere. Variation of the documented LDG through time resulted primarily from fluctuations in annual sea-surface temperature and long-term climate changes.
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Registered trials
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