Zobrazeno 1 - 10
of 39
pro vyhledávání: '"Cole T. Edwards"'
Autor:
Cynthia M. Liutkus-Pierce, Kevin K. Takashita-Bynum, Luke A. Beane, Cole T. Edwards, Oliver E. Burns, Sara Mana, Sidney Hemming, Aryeh Grossman, James D. Wright, Francis M. Kirera
Publikováno v:
Frontiers in Ecology and Evolution, Vol 7 (2019)
The Hominoidea (apes and, eventually, humans) and Cercopithecoidea (Old World monkeys) diverged from a common ancestor during the late Oligocene (~25 Ma) in East Africa. Subsequently, both catarrhine groups diversified in the early Miocene (~23-16 Ma
Externí odkaz:
https://doaj.org/article/c5a63eaa212549898186e568bf83b035
Publikováno v:
Geological Society, London, Special Publications. 532:137-156
Tracking climatic changes throughout the Ordovician is crucial to a better understanding of the coevolution of life and environment on Earth. Ordovician climate fluctuations have been the subject of a vigorous and productive body of work over the pas
Publikováno v:
Geochimica et Cosmochimica Acta. 341:116-131
Autor:
Christopher T. Conwell, Matthew R. Saltzman, Cole T. Edwards, Elizabeth M. Griffith, Y. Datu Adiatma
Publikováno v:
Geology. 50:886-890
It remains unclear whether waning of the volcanic degassing CO2 source or enhancement of the mafic (Ca, Mg-silicate) weathering CO2 sink, or both, caused global cooling leading to the Ordovician greenhouse–icehouse transition. We present a uniquely
Publikováno v:
GSA Bulletin. 134:261-274
The oxygen isotopic compositions (δ18O) of minimally altered phosphate minerals and fossils, such as conodont elements, are used as a proxy for past ocean temperature. Phosphate is thermally stable under low to moderate burial conditions and is idea
Autor:
Cole T Edwards
Table S1: Stable oxygen isotopic data of each conodont measured using SIMS; Table S2: Stable oxygen isotopic data using SIMS of the Durango apatite standard and a modern shark tooth; Figure S1: Cross plot of d18Omean values and OH/16O from the Shingl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::41ca1d9ef4fa2b879e86bdff0f71b81c
https://doi.org/10.1130/gsab.s.14356757
https://doi.org/10.1130/gsab.s.14356757
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 530:249-270
The Ordovician Period records an extraordinary biodiversity increase known as the Great Ordovician Biodiversification Event (GOBE), which coincided with a series of environmental changes to the Earth System, notably a cooling global ocean, increased
Autor:
Cole T. Edwards
Publikováno v:
Palaeoworld. 28:37-50
The Great Ordovician Biodiversification Event (GOBE) represents a four-fold increase of genus-level diversity that post-dates the diversification of the ‘Cambrian explosion’ by 40–50 Myr. A major increase in atmospheric oxygen (O2) levels is th
Autor:
Cole T. Edwards, David R. Cole, J. Sheets, Susan A. Welch, Matthew Place, Matthew R. Saltzman, Neeraj Gupta
Publikováno v:
Applied Geochemistry. 100:380-392
The Dover 33 Reef, part of the Niagaran Reef Complex in Northern Michigan (USA), has been the focus of an enhanced oil recovery/carbon capture utilization and storage (EOR/CCUS) project as part of the Phase III-Midwest Regional Carbon Sequestration P
Publikováno v:
Geological Society of America Abstracts with Programs.