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Bridget S. Wade

Researcher at University College London

Publications -  134
Citations -  6416

Bridget S. Wade is an academic researcher from University College London. The author has contributed to research in topics: Foraminifera & Paleogene. The author has an hindex of 36, co-authored 129 publications receiving 5443 citations. Previous affiliations of Bridget S. Wade include Rutgers University & University of Edinburgh.

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Review and revision of Cenozoic tropical planktonic foraminiferal biostratigraphy and calibration to the geomagnetic polarity and astronomical time scale

TL;DR: In this article, an amended low-latitude (tropical and subtropical) Cenozoic planktonic foraminiferal zonation is presented, based on the first appearance dates of Globigerinatheka kugleri and Hantkenina singanoae.
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The Heartbeat of the Oligocene Climate System

TL;DR: A 13-million-year continuous record of Oligocene climate from the equatorial Pacific reveals a pronounced “heartbeat” in the global carbon cycle and periodicity of glaciations.
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Atmospheric carbon dioxide through the Eocene–Oligocene climate transition

TL;DR: The results confirm the central role of declining in the development of the Antarctic ice sheet (in broad agreement with carbon cycle modelling) and help to constrain mechanisms and feedbacks associated with the Earth’s biggest climate switch of the past 65 Myr.
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Stable warm tropical climate through the Eocene Epoch

TL;DR: In this paper, the authors present paleotemperature estimates from foraminifer isotopes and the membrane lipids of marine Crenarcheota from new drill cores in Tanzania that indicate a warm and generally stable tropical climate over this period.
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A Cenozoic record of the equatorial Pacific carbonate compensation depth

Heiko Pälike, +70 more
- 30 Aug 2012 - 
TL;DR: A carbonate accumulation record that covers the past 53 million years from a depth transect in the equatorial Pacific Ocean is presented and large superimposed fluctuations in carbonate compensation depth are found during the middle and late Eocene.