Paleoceanography and Paleoclimatology

Papers
(The H4-Index of Paleoceanography and Paleoclimatology is 18. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-02-01 to 2025-02-01.)
ArticleCitations
Assessing Seasonal and Inter‐Annual Marine Sediment Climate Proxy Data221
Capturing Equatorial Pacific Variability With Multivariate Sr‐U Coral Thermometry69
Strong Climate Control on the Millennial‐Scale Dust Variability and Sediment Provenances in the Equatorial Indian Ocean Inferred From Sr‐Nd Isotopes32
Planktic Foraminiferal Resilience to Environmental Change Associated With the PETM31
Dynamics of the Marine Dissolved Organic Carbon Reservoir in Glacial Climate Simulations: The Importance of Biological Production29
Warming and Carbon Injection at the Paleocene‐Eocene Boundary: Bayesian Modeling Supports Synchroneity26
Impact of Dust and Temperature on Primary Productivity in Late Miocene Oceans25
The Timing of the Middle Pleistocene Glacial Terminations Based on 40Ar/39Ar Detrital Sanidine Dating25
Multi‐Year ENSO Events Over the Last Two Millennia25
Increased Productivity in the Equatorial Pacific During the Deglaciation Inferred From the Ba/Ca Ratios of Non‐Spinose Planktic Foraminifera24
Influence of the Late Ordovician‐Early Silurian Paleoenvironment and Related Geological Processes on the Organic Matter Accumulation and Carbon Isotope Excursion24
Cenozoic Proxy Constraints on Earth System Sensitivity to Greenhouse Gases22
Biomarker and Pollen Evidence for Late Pleistocene Pluvials in the Mojave Desert20
Climate Variations in the Past 250 Million Years and Contributing Factors20
Thank You to Our 2022 Peer Reviewers20
Issue Information20
Issue Information19
18
A Multicentennial Proxy Record of Northeast Pacific Sea Surface Temperatures From the Annual Growth Increments of Panopea generosa18
Interactions of the Westerlies and Asian Summer Monsoon Since the Last Deglaciation in the Northeastern Qinghai‐Tibet Plateau18
18
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