Zobrazeno 1 - 10
of 74
pro vyhledávání: '"JOHN S. COMPTON"'
Publikováno v:
South African Journal of Geology. 124:1007-1032
High-resolution mapping, sampling and analysis of upper Quaternary southern African continental margin sediments recovered from beyond the Last Glacial Maximum shoreline (>130 m water depth) have expanded our understanding of how marine and terrestri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba7385062d989601b008ed174c40703d
https://doi.org/10.25131/sajg.124.0059
https://doi.org/10.25131/sajg.124.0059
Autor:
EUGENE W. BERGH, JOHN S. COMPTON
Publikováno v:
Zootaxa. 5091(1)
Middle Miocene foraminifera from the northern Namibian outer continental shelf are indicators of a period prior to the initiation of the Benguela Upwelling System (BUS). This study provides an update to the occurrence and taxonomy of Miocene foramini
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7a55bb34b33c780738ec99ed337e466f
https://pubmed.ncbi.nlm.nih.gov/35391261
https://pubmed.ncbi.nlm.nih.gov/35391261
Autor:
Eugene W. Bergh, John S. Compton
Publikováno v:
Marine Micropaleontology. 177:102180
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::692faf020dfe59846299701faf72398f
https://doi.org/10.1016/j.marmicro.2022.102180
https://doi.org/10.1016/j.marmicro.2022.102180
The Meridional Overturning Circulation is crucial in regulating Earth‘s climate and is composed of various ocean currents, playing an important role in heat exchange and the distribution of water masses. The transfer of water masses also affects re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b6200f979368df2ffa36c756c0a6a899
https://doi.org/10.5194/egusphere-egu2020-85
https://doi.org/10.5194/egusphere-egu2020-85
Publikováno v:
Quaternary Science Reviews. 201:303-318
Sea-level change around southern Africa (southern Namibia, South Africa, southern Mozambique) since Termination I has been quantified using a variety of indicators. Existing and new data are reviewed to provide a baseline for future studies and ident
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dc5c3e4938f71eb6e2ecf7ad585916ae
https://doi.org/10.1016/j.quascirev.2018.10.013
https://doi.org/10.1016/j.quascirev.2018.10.013
Publikováno v:
Journal of African Earth Sciences. 141:33-48
Middle Miocene to Plio-Pleistocene foraminifera provide insights into the palaeoenvironment on the northern Namibian continental shelf located at the far northern end of the present-day Benguela Upwelling System (BUS). Biostratigraphy and Strontium I
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91c5c520d6aed169c2a5b749e88ce367
https://doi.org/10.1016/j.jafrearsci.2018.01.018
https://doi.org/10.1016/j.jafrearsci.2018.01.018
Autor:
Panagiotis Karkanas, John S. Compton, Zenobia Jacobs, Erich C. Fisher, Hayley C. Cawthra, Curtis W. Marean
Publikováno v:
Quaternary Science Reviews. 181:156-172
Pleistocene shoreline deposits comprised of calcified shallow marine (palaeobeach) and aeolian (palaeodune) facies found along mid-latitude coastlines can be useful indicators of past sea levels. Here, we describe a succession of such deposits that a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52b014bae4dc8f0ca056e486f4b5e7c4
https://doi.org/10.1016/j.quascirev.2017.12.002
https://doi.org/10.1016/j.quascirev.2017.12.002
Autor:
Eugene W. Bergh, John S. Compton
Publikováno v:
Palaeontologia Electronica.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::496072a3b5b211b151676b3521cd6923
https://doi.org/10.26879/1018
https://doi.org/10.26879/1018
Autor:
Peter Frenzel, Hayley C. Cawthra, Matthias Zabel, John S. Compton, Lukas Gander, Annette Hahn
The continental shelf of the Palaeo-Agulhas Plain (PAP) is scattered with Pleistocene deposits with subdued topography. Their exaggerated lateral extension is the expression of a flat underlying substrate and availability of accommodation space, depo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::841106c8cfebf79d1336ff9bba1c3830
https://doi.org/10.7287/peerj.preprints.27757v1
https://doi.org/10.7287/peerj.preprints.27757v1
Autor:
John S. Compton, Eugene W. Bergh
Publikováno v:
Marine Geology. 380:290-314
Phosphorite deposits provide a source of fertilizer to feed an increasingly populated world and they provide a record of paleoceanographic changes in upwelling systems linked to climate. The Benguela Upwelling System (BUS) is among the most productiv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3edfa386ae4c86d243f4e64b03b69ce2
https://doi.org/10.1016/j.margeo.2016.04.006
https://doi.org/10.1016/j.margeo.2016.04.006