Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Tim C. Sweere"'
Autor:
Alexander J. Dickson, Hugh C. Jenkyns, Erdem Idiz, Tim C. Sweere, Melissa J. Murphy, Sander H. J. M. van den Boorn, Micha Ruhl, James S. Eldrett, Donald Porcelli
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 3, Pp n/a-n/a (2021)
Abstract Intervals of extreme warmth are predicted to drive a decrease in the oxygen content of the oceans. This prediction has been tested for the acme of short (
Externí odkaz:
https://doaj.org/article/c854fd9d2f794f62b8bd2eee45f42ddd
Autor:
Derek Vance, Morten B. Andersen, Tim C. Sweere, Zhiwei He, Matthew O Clarkson, Alex Guthauser, Fang Huang, Corey Archer, Peter Kraal
Publikováno v:
Geochimica et Cosmochimica Acta, 309
The abundances and isotope compositions of molybdenum (Mo) and uranium (U) in ancient sediments are promising tracers of the redox state of the past ocean, whose basis lies in the environmentally dependent Mo and U isotope signatures in modern oceani
Publikováno v:
Geobiology, 21 (3)
Nickel and zinc are both bio-essential micronutrients with a nutrient-like distribution in the modern ocean, but show key differences in their biological functions and geochemical behavior. Eukaryotic phytoplankton, and especially diatoms, have high
Autor:
Alex Dickson, Don Porcelli, Tim C. Sweere, Melissa J. Murphy, Sander H. J. M. van den Boorn, Erdem Idiz, Hugh C. Jenkyns, James S Eldrett, Micha Ruhl, Gideon M. Henderson
Publikováno v:
Geochimica et Cosmochimica Acta. 287:251-262
The isotopic composition of Cd buried in marine sediments may preserve valuable palaeoenvironmental information on past ocean redox conditions or biological cycling. It is unclear, however, how the Cd-isotope composition of the sedimentary record ref
This study uses organic-rich sediments from the Tarfaya Basin, Morocco, to assess the Cd- and Zn-isotope response to dramatic global palaeoenvironmental change during the Cenomanian–Turonian interval (Late Cretaceous). These organic-rich continenta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9953deefaa5afedab7467fc3e7effdc6
https://ora.ox.ac.uk/objects/uuid:294b936b-9f01-46a8-bdfb-8d6f376e5e87
https://ora.ox.ac.uk/objects/uuid:294b936b-9f01-46a8-bdfb-8d6f376e5e87
Publikováno v:
Goldschmidt2021 abstracts.
Autor:
Tim C. Sweere, Rick Hennekam, Peter Kraal, Gert-Jan Reichart, Zeynep Erdem, Kristin Anna Ungerhofer
Publikováno v:
Goldschmidt2021 abstracts.
Autor:
Sander H. J. M. van den Boorn, Gideon M. Henderson, Don Porcelli, Maya Elrick, Tim C. Sweere, Alex Dickson, Hugh C. Jenkyns
Publikováno v:
Geology. 46(5)
Widespread deposition of organic-rich shales during the Late Cretaceous Oceanic Anoxic Event 2 (OAE 2, ca. 94 Ma) occurred during a period of significant global paleo-environmental and geochemical change. It has been proposed that an increase in nutr
Publikováno v:
Chemical Geology, 441, 235. Elsevier
Trace metal enrichments in sedimentary deposits are of prime interest because they are governed by processes that also control the production and preservation of organic matter. Consequently, trace metals have been used in reconstructions of the (pal