Zobrazeno 1 - 10
of 229
pro vyhledávání: '"D. Hemingway"'
Clay hydroxyl isotopes show an enhanced hydrologic cycle during the Paleocene-Eocene Thermal Maximum
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-10 (2022)
Novel measurements of clay hydroxyl isotopic composition show an enhanced hydrological cycle during a period of intense global warming at the Paleocene-Eocene boundary 55.9 million years ago.
Externí odkaz:
https://doaj.org/article/e9c2870f23f249ea8756a856819648bf
Publikováno v:
Biogeosciences, Vol 14, Pp 5099-5114 (2017)
Serial oxidation coupled with stable carbon and radiocarbon analysis of sequentially evolved CO2 is a promising method to characterize the relationship between organic carbon (OC) chemical composition, source, and residence time in the environment
Externí odkaz:
https://doaj.org/article/0d25a0b1e34f483eaf69dcbb9eac5aa8
Autor:
William D. Orsi, Marco J. L. Coolen, Cornelia Wuchter, Lijun He, Kuldeep D. More, Xabier Irigoien, Guillem Chust, Carl Johnson, Jordon D. Hemingway, Mitchell Lee, Valier Galy, Liviu Giosan
Publikováno v:
Scientific Reports, Vol 7, Iss 1, Pp 1-12 (2017)
Abstract Selection of microorganisms in marine sediment is shaped by energy-yielding electron acceptors for respiration that are depleted in vertical succession. However, some taxa have been reported to reflect past depositional conditions suggesting
Externí odkaz:
https://doaj.org/article/3bc74f0f1e6e4bb9a8ac21a3fe65b03b
Autor:
Andrew R. Shaughnessy, Michael J. Forgeng, Tao Wen, Xin Gu, Jordon D. Hemingway, Susan L. Brantley
Publikováno v:
Water Resources Research, 59 (5)
As drinking-water scarcity grows worldwide, we need to improve predictions of the quantity and quality of our water resources. An overarching problem for model improvement is that we do not know the geological structure of aquifers in sufficient deta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b5b72b07e9ad59040f0fcee42e024594
https://hdl.handle.net/20.500.11850/615083
https://hdl.handle.net/20.500.11850/615083
Autor:
Gordon N. Inglis, Tripti Bhattacharya, Jordon D. Hemingway, Emily H. Hollingsworth, Sarah J. Feakins, Jessica E. Tierney
Publikováno v:
Annual Review of Earth and Planetary Sciences. 50:369-394
The response of the terrestrial biosphere to warming remains one of the most poorly understood and quantified aspects of the climate system. One way to test the behavior of the Earth system in warm climate states is to examine the geological record.
Publikováno v:
Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta, 324
Geochimica et Cosmochimica Acta, 324
The triple-oxygen isotope (17O/16O, 18O/16O) measurement of oxygen-bearing species represents one of the most robust tools to directly trace oxygen cycling in the environment. One particularly consequential application of this isotope system is the a
Autor:
Felix J. Elling, Thomas W. Evans, Vinitra Nathan, Jordon D. Hemingway, Jenan J. Kharbush, Barbara Bayer, Eva Spieck, Fatima Husain, Roger E. Summons, Ann Pearson
Publikováno v:
Geobiology. 20:399-420
Hopanoid lipids, bacteriohopanols and bacteriohopanepolyols, are membrane components exclusive to bacteria. Together with their diagenetic derivatives, they are commonly used as biomarkers for specific bacterial groups or biogeochemical processes in
Publikováno v:
PNAS Nexus, 1 (5)
The biogeochemical fluxes that cycle oxygen (O2) play a critical role in regulating Earth’s climate and habitability. Triple-oxygen isotope (TOI) compositions of marine dissolved O2 are considered a robust tool for tracing oxygen cycling and quanti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cf645559624aa355ebb042f869fe75ab
https://hdl.handle.net/20.500.11850/592716
https://hdl.handle.net/20.500.11850/592716
Autor:
Eva Spieck, Jordon D. Hemingway, Felix J Elling, Roger E. Summons, Jenan J. Kharbush, Thomas W. Evans, Ann Pearson
Publikováno v:
Proc Natl Acad Sci U S A
Bacterial hopanoid lipids are ubiquitous in the geologic record and serve as biomarkers for reconstructing Earth’s climatic and biogeochemical evolution. Specifically, the abundance of 2-methylhopanoids deposited during Mesozoic ocean anoxic events
Autor:
Nathan Looser, Paul Petschnig, Jordon D. Hemingway, Alvaro Fernandez, Luiz Grafulha Morales, Alberto Perez-Huerta, Madeleine L. Vickers, Gregory D. Price, Max W. Schmidt, Stefano M. Bernasconi
Publikováno v:
SSRN Electronic Journal.