Zobrazeno 1 - 10
of 44
pro vyhledávání: '"Jessica R. Creveling"'
Autor:
J. A. Mattias Green, Hannah S. Davies, Joao C. Duarte, Jessica R. Creveling, Christopher Scotese
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-7 (2020)
How and why the ‘Snowball Earth’ occurred during the Cryogenian period is debated. Here, the authors show that the cryogenian ocean hosted diminished tidal amplitudes and associated energy dissipation rates, reaching 10-50% of today’s rates thu
Externí odkaz:
https://doaj.org/article/5021c8e0c75e455faa0cf1e07ca3bbf4
Autor:
Meghan E. King, Jessica R. Creveling
Publikováno v:
Geology. 50:923-928
Glacial isostatic adjustment (GIA) imparts geographic variability in the amplitude and timing of local sea-level (LSL) change arising from glacial-interglacial oscillations relative to a global mean signal (eustasy). We modeled how GIA manifests in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aef8be1737ed28971bf8341e9d4d3825
https://doi.org/10.1130/g49841.1
https://doi.org/10.1130/g49841.1
A global database of marine isotope substage 5a and 5c marine terraces and paleoshoreline indicators
Publikováno v:
Earth System Science Data, Vol 13, Pp 3467-3490 (2021)
In this review we compile and document the elevation, indicative meaning, and chronology of marine isotope substage 5a and 5c sea level indicators for 39 sites within three geographic regions: the North American Pacific coast, the North American Atla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::94a8f5f5836901b898fc56d3e9447fbb
https://doi.org/10.5194/essd-13-3467-2021
https://doi.org/10.5194/essd-13-3467-2021
Autor:
Jessica R. Creveling, Meghan E. King
Supplemental figures showing depth site relative sea-level histories and stratigraphic surface ages; and tables of the mean count, thickness, and water-depth change of systems tracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ae18f21bcabc44e05a2701a39210f8ac
https://doi.org/10.1130/geol.s.19601872
https://doi.org/10.1130/geol.s.19601872
Autor:
Jessica R. Creveling, Christopher R. Scotese, J. A. Mattias Green, João C. Duarte, Hannah Davies
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-7 (2020)
Nature Communications
Nature Communications
The severe “Snowball Earth” glaciations proposed to have existed during the Cryogenian period (720 to 635 million years ago) coincided with the breakup of one supercontinent and assembly of another. Whereas the presence of extensive continental i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3fea4b3e307f40f9650d0d750e46c459
https://doaj.org/article/5021c8e0c75e455faa0cf1e07ca3bbf4
https://doaj.org/article/5021c8e0c75e455faa0cf1e07ca3bbf4
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:13354-13366
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4810fa33ce1af0a77b43f917ad946be2
https://doi.org/10.1029/2019jb018489
https://doi.org/10.1029/2019jb018489
Autor:
Linda Pan, E. M. Powell, Konstantin Latychev, Jessica R. Creveling, Peter U. Clark, Mark Hoggard, Natalya Gomez, Jerry X. Mitrovica
Publikováno v:
Science Advances
Rapid uplift of marine sectors exposed by WAIS collapse amplified GMSL rise in the past and will do so in the future.
Geodetic, seismic, and geological evidence indicates that West Antarctica is underlain by low-viscosity shallow mantle. Thus, a
Geodetic, seismic, and geological evidence indicates that West Antarctica is underlain by low-viscosity shallow mantle. Thus, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4e94991671043f2d10a9a740382c19e3
https://doi.org/10.1126/sciadv.abf7787
https://doi.org/10.1126/sciadv.abf7787
Autor:
E. M. Powell, Natalya Gomez, Linda Pan, Mark Hoggard, Konstantin Latychev, Jerry X. Mitrovica, Jessica R. Creveling, Peter U. Clark
Studies of peak global mean sea level (GMSL) during the Last Interglacial (LIG; 130-116 ka) commonly cite values ranging from ~2-5 m for the maximum contribution from grounded, marine-based sectors of the West Antarctic Ice Sheet (WAIS). However, thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a8dec6163f580f05b29305d9d0326a98
https://doi.org/10.5194/egusphere-egu21-13786
https://doi.org/10.5194/egusphere-egu21-13786
Reconstructions of global mean sea level (GMSL) through interstadials such as Marine Isotope Stages (MIS) 5a and 5c provide important constraints on the rates of growth and collapse of major ice sheets during warm periods analogous to future climate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::521c87f7ff4eaad6cdfa947e6b9b5859
https://doi.org/10.5194/egusphere-egu21-16399
https://doi.org/10.5194/egusphere-egu21-16399
The severe “Snowball Earth” glaciations proposed to have existed during the Cryogenian period (720 to 635 million years ago) coincided with the breakup of one supercontinent (Rodinia) and assembly of another (Pannotia). The presence of extensive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e6f520e4ee195c498cc90f08e705d3b
https://doi.org/10.5194/egusphere-egu21-1354
https://doi.org/10.5194/egusphere-egu21-1354