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Stable isotope chemistry of fossil bone as a new paleoclimate indicator
Matthew J. Kohn
, J. Mclver Law
Geosciences Department
University of South Carolina
Research output
:
Contribution to journal
›
Article
›
peer-review
80
Scopus citations
Overview
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Keyphrases
C Isotopes
100%
Paleoclimate
100%
Fossil Bone
100%
Stable Isotope Chemistry
100%
Aridity
66%
O Isotopes
66%
Isotope Fractionation
66%
Mascall
66%
Bone Apatite
66%
Rattlesnake
66%
Idaho
33%
Oregon
33%
Temperature Rise
33%
Value-based
33%
Water Composition
33%
Soil Water
33%
Compositional Changes
33%
Paleosol
33%
Recrystallized
33%
Late Oligocene
33%
John Day
33%
Dry Climate
33%
Minimum Temperature
33%
Cascade Range
33%
Late Pleistocene
33%
Wet Climate
33%
Tooth Enamel
33%
Positive Deviation
33%
Meteoric Water
33%
Short-term Trend
33%
Global Warming Event
33%
Paleosols Sequences
33%
Earth and Planetary Sciences
Aridity
100%
Stable Isotope
100%
Paleosol
100%
Calcium Phosphate
100%
Oligocene
100%
Paleoclimate
100%
Fossil bone
100%
Idaho
50%
Late Pleistocene
50%
Soil Water
50%
Oregon
50%
Meteoric Water
50%
Global Warming
50%
Teeth
50%