Stratigraphy and sedimentary petrology of the northwest quarter of the Dutchman Butte quadrangle, southwest Oregon

Koler, T. E.

doi:10.15760/etd.3043

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2023

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“…and is high for what we consider to be a reasonable surface temperature but is consistent with recrystallization at depth in the subsurface in warmer temperatures before subsequent uplift. Indeed, the John Day Fault, which is proximal to the Mascall Formation (the origin of the sample, Oregon), underwent uplift, producing the Strawberry-Aldrich Mountains, during the Pliocene (Kuiper, 1988). The exact thermal history of the Celtis willistoni fossil has not been published, but the temperature is consistent with recrystallization at depth.…”

Section: Diagenesismentioning

confidence: 99%

Clumped Isotope Thermometry in Plant‐Derived Carbonates

Stein

Turner

Amundson

et al. 2023

Paleoceanog and Paleoclimatol

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Reconstructions of past terrestrial climates are used to understand the temporal evolution and drivers of Earth's surface climate and serve as benchmarks for evaluating models of potential future climate scenarios (e.g., Tierney et al., 2020). In terrestrial systems, past climate variables of interest can be estimated using a variety of proxies including: Reconstructions of past near-surface temperatures based on, for example, fossil assemblages (such as nearest living relative techniques and leaf physiognomy), the isotopic composition of pedogenic carbonates, and pedogenic weathering indices (e.g.,

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Section: Diagenesismentioning

confidence: 99%