Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Andrew O. Parker"'
Autor:
Zane R. Jobe, Ciarán J. O’Byrne, R. D. A. Smith, Andrew O. Parker, Alessandro Cantelli, Zoltán Sylvester, Niall C. Slowey, Matthew A. Wolinsky, Carlos Pirmez, Nick Howes, Brad E. Prather
Publikováno v:
Geological Society of America Bulletin. 129:23-37
Near-seafloor core and seismic-reflection data from the western Niger Delta continental slope document the facies, architecture, and evolution of submarine channel and intraslope submarine fan deposits. The submarine channel enters an 8 km long x 8 k
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c4f67a9563fbdc9954b346b37be56f85
https://doi.org/10.1130/b31440.1
https://doi.org/10.1130/b31440.1
Publikováno v:
Paleoceanography. 30:1425-1436
The role of Atlantic Meridional Overturning Circulation (AMOC) as the driver of Dansgaard-Oeschger (DO) variability that characterized Marine Isotope Stage 3 (MIS 3) has long been hypothesized. Although there is ample proxy evidence suggesting that D
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d99d56acfa7a105877bb5fbba7a4298c
https://doi.org/10.1002/2015pa002832
https://doi.org/10.1002/2015pa002832
Publikováno v:
Journal of Sedimentary Research. 85:729-753
Changes in sediment supply and caliber during the last ∼ 130 ka have resulted in a complex architectural evolution of the Y channel system on the western Niger Delta slope. This evolution consists of four phases, each with documented or inferred ch
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7987c6af2be2338dae69f1e502dc24f3
https://doi.org/10.2110/jsr.2015.30
https://doi.org/10.2110/jsr.2015.30
Publikováno v:
Scientific Reports
Scientific Reports, Vol 7, Iss 1, Pp 1-11 (2017)
Scientific Reports, Vol 7, Iss 1, Pp 1-11 (2017)
Multiple lines of evidence show that cold stadials in the North Atlantic were accompanied by both reductions in Atlantic Meridional Overturning Circulation (AMOC) and collapses of the West African Monsoon (WAM). Although records of terrestrial change
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::70b3e05eca3aca1d80d07d8957f1d4dc
http://europepmc.org/articles/PMC5684145
http://europepmc.org/articles/PMC5684145
Publikováno v:
Earth And Planetary Science Letters (0012-821X) (Elsevier Science Bv), 2016-09, Vol. 449, P. 79-88
Widespread drought characterized the Heinrich 1 and Younger Dryas cold periods of the last deglaciation throughout much of Africa, causing large increases in dust emissions from the Sahara and Sahel. At the same time, increases in wind strength may h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2fd295dc0ca186987ff7e72b9f8c0a53
https://archimer.ifremer.fr/doc/00421/53223/
https://archimer.ifremer.fr/doc/00421/53223/
