ArticlePaleoceanography and paleoclimatology2021
Investigating Mesozoic Climate Trends and Sensitivities With a Large Ensemble of Climate Model Simulations.
Article in Paleoceanography and paleoclimatology, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.
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Who cites it
9 citing papers in PubMed.
- Transitions between persistent climate-carbon regimes coincide with elevated Phanerozoic biosphere vulnerability.Nature communications · 2026Article
- Earliest Jurassic plant assemblages from Sweden reveal a low-diversity ginkgoalean and cheirolepid flora dominating the post-extinction landscape.Annals of botany · 2026Article
- Tectonic-astronomical interactions in shaping late Paleozoic climate and organic carbon burial.Nature communications · 2025Article
- Back to an ice-free future: Early Cretaceous seasonal cycles of sea surface temperature and glacier ice.Science advances · 2025Article
- Global latitudinal gradients and the evolution of body size in dinosaurs and mammals.Nature communications · 2024Article
- Modes of Pangean lake level cyclicity driven by astronomical climate pacing modulated by continental position andProceedings of the National Academy of Sciences of the United States of America · 2022Article
- Arctic ice and the ecological rise of the dinosaurs.Science advances · 2022Article
- A high-resolution climate simulation dataset for the past 540 million years.Scientific data · 2022Article
- Investigating Mesozoic Climate Trends and Sensitivities With a Large Ensemble of Climate Model Simulations.Paleoceanography and paleoclimatology · 2021Article
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Authors and funding
5 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The Mesozoic era (∼252 to 66 million years ago) was a key interval in Earth's evolution toward its modern state, witnessing the breakup of the supercontinent Pangaea and significant biotic innovations like the early evolution of mammals. Plate tectonic dynamics drove a fundamental climatic transition from the early Mesozoic supercontinent toward the Late Cretaceous fragmented continental configuration. Here, key aspects of Mesozoic long-term environmental changes are assessed in a climate model ensemble framework. We analyze so far the most extended ensemble of equilibrium climate states simulated for evolving Mesozoic boundary conditions covering the period from 255 to 60 Ma in 5 Myr timesteps. Global mean temperatures are generally found to be elevated above the present and exhibit a baseline warming trend driven by rising sea levels and increasing solar luminosity. Warm (Triassic and mid-Cretaceous) and cool (Jurassic and end-Cretaceous) anomalies result from pCO
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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.