Chemostratigraphic implications of spatial variation in the Paleocene‐Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
AA Baczynski, FA McInerney, SL Wing… - Geochemistry …, 2013 - Wiley Online Library
The Paleocene‐Eocene Thermal Maximum (PETM) is marked by a prominent negative
carbon isotope excursion (CIE) of 3–5‰ that has a characteristic rapid onset, stable body …
carbon isotope excursion (CIE) of 3–5‰ that has a characteristic rapid onset, stable body …
Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
A Baczynski, F McInerney, S Wing, M Kraus… - 2013 - hekyll.services.adelaide.edu.au
[1] The Paleocene-Eocene Thermal Maximum (PETM) is marked by a prominent negative
carbon isotope excursion (CIE) of 3–5‰ that has a characteristic rapid onset, stable body …
carbon isotope excursion (CIE) of 3–5‰ that has a characteristic rapid onset, stable body …
Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
A Baczynski, F McInerney, S Wing, M Kraus, J Bloch… - 2013 - digital.library.adelaide.edu.au
[1] The Paleocene-Eocene Thermal Maximum (PETM) is marked by a prominent negative
carbon isotope excursion (CIE) of 3–5‰ that has a characteristic rapid onset, stable body …
carbon isotope excursion (CIE) of 3–5‰ that has a characteristic rapid onset, stable body …
[引用][C] Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
AA Baczynski, FA McInerney… - Geochemistry …, 2013 - espace.library.uq.edu.au
The Paleocene-Eocene Thermal Maximum (PETM) is marked by a prominent negative
carbon isotope excursion (CIE) of 3-5‰ that has a characteristic rapid onset, stable body …
carbon isotope excursion (CIE) of 3-5‰ that has a characteristic rapid onset, stable body …
[PDF][PDF] Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
AA Baczynski, FA McInerney, SL Wing, MJ Kraus… - 2013 - researchgate.net
[2] The Paleocene-Eocene epoch boundary at $56 Ma is marked by a significant
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …
Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
AA Baczynski, FA McInerney, SL Wing… - Geochemistry …, 2013 - ui.adsabs.harvard.edu
Abstract The Paleocene-Eocene Thermal Maximum (PETM) is marked by a prominent
negative carbon isotope excursion (CIE) of 3-5‰ that has a characteristic rapid onset, stable …
negative carbon isotope excursion (CIE) of 3-5‰ that has a characteristic rapid onset, stable …
[PDF][PDF] Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
AA Baczynski, FA McInerney, SL Wing, MJ Kraus… - 2013 - people.duke.edu
[2] The Paleocene-Eocene epoch boundary at $56 Ma is marked by a significant
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …
[PDF][PDF] Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
AA Baczynski, FA McInerney, SL Wing, MJ Kraus… - 2013 - academia.edu
[2] The Paleocene-Eocene epoch boundary at $56 Ma is marked by a significant
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …
[PDF][PDF] Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
AA Baczynski, FA McInerney, SL Wing, MJ Kraus… - 2013 - academia.edu
[2] The Paleocene-Eocene epoch boundary at $56 Ma is marked by a significant
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …
[PDF][PDF] Chemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, Wyoming
AA Baczynski, FA McInerney, SL Wing, MJ Kraus… - 2013 - people.duke.edu
[2] The Paleocene-Eocene epoch boundary at $56 Ma is marked by a significant
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …
perturbation to the global carbon cycle. The release of thousands of gigatons of isotopically …