K
Kyger C. Lohmann
Researcher at University of Michigan
Publications - 145
Citations - 10824
Kyger C. Lohmann is an academic researcher from University of Michigan. The author has contributed to research in topics: Calcite & Diagenesis. The author has an hindex of 54, co-authored 144 publications receiving 10112 citations. Previous affiliations of Kyger C. Lohmann include Stony Brook University & University of Iowa.
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Journal ArticleDOI
Evolution of Early Cenozoic marine temperatures
TL;DR: In this paper, the equator to high southern latitude sea surface and vertical temperature gradients are reconstructed from oxygen isotope values of planktonic and benthic foraminifers.
Book ChapterDOI
Geochemical Patterns of Meteoric Diagenetic Systems and Their Application to Studies of Paleokarst
TL;DR: The isotopic and cation chemistry of meteoric waters changes in response to the effects of rock-water interaction, uptake of organically derived CO2, and primary mineralogic differences among carbonate terranes as discussed by the authors.
Journal ArticleDOI
Abrupt climate change and transient climates during the Paleogene: a marine perspective.
TL;DR: It is investigated the possibility that sudden reorganizations in ocean and/or atmosphere circulation during these abrupt transitions generated short-term positive feedbacks that briefly sustained these transient climatic states.
Journal ArticleDOI
Controls on the stable isotope composition of seasonal growth bands in aragonitic fresh-water bivalves (unionidae)
TL;DR: The final full year of shell growth in 3 unionids collected in 1992 from two southern Michigan rivers was sampled for stable isotope analysis with a resolution of 30 μm as discussed by the authors.
Journal ArticleDOI
Spatial distribution and seasonal variation in 18O/16O of modern precipitation and river water across the conterminous USA
Andrea Dutton,Andrea Dutton,Bruce H. Wilkinson,Jeffrey M. Welker,Gabriel J. Bowen,Kyger C. Lohmann +5 more
TL;DR: In this paper, the authors report a quantitative analysis of regional differences in the oxygen isotope composition of river water and precipitation across the USA because data are now available to undertake a more geographically and temporally extensive analysis than was formerly possible.