Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Samantha C. Carter"'
Autor:
Samantha C. Carter, Elizabeth M. Griffith, Theresa A. Jorgensen, Karin G. Coifman, W. Ashley Griffith
Publikováno v:
Communications Earth & Environment, Vol 2, Iss 1, Pp 1-7 (2021)
The prospect of working outdoors, which has commonly been emphasized in geoscience recruitment, is less attractive to students than altruistic factors when considering future career paths, according to a survey of students in a diverse southwestern U
Externí odkaz:
https://doaj.org/article/d26b2259774041f1aff5d160e652fb79
Publikováno v:
Minerals, Vol 10, Iss 5, p 421 (2020)
Marine barite (BaSO4) is a relatively ubiquitous, though minor, component of ocean sediments. Modern studies of the accumulation of barite in ocean sediments have demonstrated a robust correlation between barite accumulation rates and carbon export t
Externí odkaz:
https://doaj.org/article/8ad19405a04b4e81bc6efde2a6ab578d
Autor:
Karin G. Coifman, W. Ashley Griffith, Elizabeth M. Griffith, Theresa A. Jorgensen, Samantha C. Carter
Publikováno v:
Communications Earth & Environment, Vol 2, Iss 1, Pp 1-7 (2021)
A common approach to attract students in the United States to the geosciences is to emphasize outdoor experiences in the natural world. However, it is unclear how successful this strategy is. Specifically, the geosciences have been less successful th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e49cb000b6d506f081c3905f48da7766
https://doaj.org/article/d26b2259774041f1aff5d160e652fb79
https://doaj.org/article/d26b2259774041f1aff5d160e652fb79
Autor:
Howie D. Scher, Samantha C. Carter, Timothy M. Dellapenna, Peter D. Clift, Elizabeth M. Griffith
Publikováno v:
Geological Magazine. 157:879-894
Reconstructing the provenance of siliciclastic marine sediment is important for understanding sediment pathways and constraining palaeoclimate and erosion records. However, physical fractionation of different size fractions can occur during sediment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eca2f06e327e6f479ec86256bd8f5e63
https://doi.org/10.1017/s0016756820000394
https://doi.org/10.1017/s0016756820000394
Publikováno v:
Goldschmidt2021 abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1205491974fd10bf248130df87272127
https://doi.org/10.7185/gold2021.7706
https://doi.org/10.7185/gold2021.7706
Publikováno v:
Geology. 44:923-926
The middle Miocene climate transition (MMCT) is characterized by an abrupt 1‰ increase in benthic foraminiferal oxygen isotopes at ca. 13.8 Ma, marking expansion of the Antarctic Ice Sheet and transition of Earth9s climate to a cooler, relatively s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a65a4f64bfd3a003aceb1b07648737c
https://doi.org/10.1130/g38290.1
https://doi.org/10.1130/g38290.1
