ArticlePaleoceanography and paleoclimatology2020
A Warm, Stratified, and Restricted Labrador Sea Across the Middle Eocene and Its Climatic Optimum.
Article in Paleoceanography and paleoclimatology, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
5 citing papers in PubMed, 26 citations in OpenAlex.
- What the geological past can tell us about the future of the ocean's twilight zone.Nature communications · 2023Article
- North Atlantic surface ocean warming and salinization in response to middle Eocene greenhouse warming.Science advances · 2023Article
- Article
- Slow-growing reef corals as climate archives: A case study of the Middle Eocene Climatic Optimum 40 Ma ago.Science advances · 2022Article
- A Warm, Stratified, and Restricted Labrador Sea Across the Middle Eocene and Its Climatic Optimum.Paleoceanography and paleoclimatology · 2020Article
Corrections and comments
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Authors and funding
14 authors at 7 institutions in 5 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Several studies indicate that North Atlantic Deep Water (NADW) formation might have initiated during the globally warm Eocene (56-34 Ma). However, constraints on Eocene surface ocean conditions in source regions presently conducive to deep water formation are sparse. Here we test whether ocean conditions of the middle Eocene Labrador Sea might have allowed for deep water formation by applying (organic) geochemical and palynological techniques, on sediments from Ocean Drilling Program (ODP) Site 647. We reconstruct a long-term sea surface temperature (SST) drop from ~30°C to ~27°C between 41.5 to 38.5 Ma, based on TEX
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Registered trials
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