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Casey Saenger

Researcher at Joint Institute for the Study of the Atmosphere and Ocean

Publications -  35
Citations -  2045

Casey Saenger is an academic researcher from Joint Institute for the Study of the Atmosphere and Ocean. The author has contributed to research in topics: Holocene & Climate change. The author has an hindex of 19, co-authored 33 publications receiving 1665 citations. Previous affiliations of Casey Saenger include United States Geological Survey & Massachusetts Institute of Technology.

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A global multiproxy database for temperature reconstructions of the Common Era

Julien Emile-Geay, +108 more
- 11 Jul 2017 - 
TL;DR: A community-sourced database of temperature-sensitive proxy records from the PAGES2k initiative, suited to investigations of global and regional temperature variability over the Common Era, and is shared in the Linked Paleo Data (LiPD) format, including serializations in Matlab, R and Python.
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Surface-temperature trends and variability in the low-latitude North Atlantic since 1552

TL;DR: For the past few centuries, multidecadal climate variability in North Atlantic sea surface temperatures has been modulated by the AMO as discussed by the authors, which is a transient climate feature that only became significant after AD 1730.
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Toward a universal carbonate clumped isotope calibration: Diverse synthesis and preparatory methods suggest a single temperature relationship

TL;DR: In this article, the authors systematically explore the impact of synthetic carbonate precipitation by replicating precipitation experiments of previous workers under a constant analytical setting, and find that the Δ47-temperature relationship does not measurably change with either the precipitation methods used in this study or acid digestion temperature.
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Carbonate clumped isotope variability in shallow water corals: Temperature dependence and growth-related vital effects

TL;DR: In this paper, the authors present a systematic survey of Δ_(47) in shallow water corals and show that the deviation from expected Δ(47) increases with calcification rate, which is inconsistent with pH-dependent changes in dissolved inorganic carbon speciation.