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Enhanced coastal paleoproductivity and nutrient supply in Upper Egypt during the Paleocene/Eocene Thermal Maximum (PETM): Mineralogical and geochemical evidence

Soliman, Mamdouh F.; Aubry, Marie-Pierre; Schmitz, Birger LU and Sherrell, Robert M. (2011) In Palaeogeography, Palaeoclimatology, Palaeoecology 310(3-4). p.365-377
Abstract
We have analyzed the geochemistry and mineralogy of the five characteristic beds that constitute the Dababiya Quarry Member (DQM) recovered from the Dababiya Quarry Core located near the Global Stratotype Section and Point (GSSP) for the base of the Eocene. Well developed in Upper Egypt, these beds are known to record the isotopic and biotic signatures of the Paleocene/Eocene thermal maximum (PETM). We have extracted the mineral phases from these beds (representing a total thickness of 2.35 m) and compared them with those of the encasing shales through qualitative and semi-quantitative SEM analysis using EDX technology. Total organic carbon was determined using the titrimetric method. Major and trace elements were analyzed using an... (More)
We have analyzed the geochemistry and mineralogy of the five characteristic beds that constitute the Dababiya Quarry Member (DQM) recovered from the Dababiya Quarry Core located near the Global Stratotype Section and Point (GSSP) for the base of the Eocene. Well developed in Upper Egypt, these beds are known to record the isotopic and biotic signatures of the Paleocene/Eocene thermal maximum (PETM). We have extracted the mineral phases from these beds (representing a total thickness of 2.35 m) and compared them with those of the encasing shales through qualitative and semi-quantitative SEM analysis using EDX technology. Total organic carbon was determined using the titrimetric method. Major and trace elements were analyzed using an inductively coupled plasma-optical emission spectrometer, and enrichment factors were established relative to Al content. We discuss the significance of our data with regard to basaltic volcanism and cometary impact, for neither of which we find support. In agreement with other studies, our data indicate very high biological productivity during the deposition of the DQM. This may be related to upwelling and/or increased nutrient supply, the latter because of an enhanced hydrologic cycle. (C) 2011 Elsevier B.V. All rights reserved. (Less)
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author
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Paleocene/Eocene Thermal Maximum (PETM), Paleoproductivity, GSSP, section, Titanomagnetite, Magnetite, Chalcophile elements
in
Palaeogeography, Palaeoclimatology, Palaeoecology
volume
310
issue
3-4
pages
365 - 377
publisher
Elsevier
external identifiers
  • wos:000296125900017
  • scopus:80053131836
ISSN
1872-616X
DOI
10.1016/j.palaeo.2011.07.027
language
English
LU publication?
yes
id
48154428-2258-4539-8e8c-ab7bc08d5678 (old id 2253128)
date added to LUP
2011-12-21 15:35:19
date last changed
2017-09-24 03:17:58
@article{48154428-2258-4539-8e8c-ab7bc08d5678,
  abstract     = {We have analyzed the geochemistry and mineralogy of the five characteristic beds that constitute the Dababiya Quarry Member (DQM) recovered from the Dababiya Quarry Core located near the Global Stratotype Section and Point (GSSP) for the base of the Eocene. Well developed in Upper Egypt, these beds are known to record the isotopic and biotic signatures of the Paleocene/Eocene thermal maximum (PETM). We have extracted the mineral phases from these beds (representing a total thickness of 2.35 m) and compared them with those of the encasing shales through qualitative and semi-quantitative SEM analysis using EDX technology. Total organic carbon was determined using the titrimetric method. Major and trace elements were analyzed using an inductively coupled plasma-optical emission spectrometer, and enrichment factors were established relative to Al content. We discuss the significance of our data with regard to basaltic volcanism and cometary impact, for neither of which we find support. In agreement with other studies, our data indicate very high biological productivity during the deposition of the DQM. This may be related to upwelling and/or increased nutrient supply, the latter because of an enhanced hydrologic cycle. (C) 2011 Elsevier B.V. All rights reserved.},
  author       = {Soliman, Mamdouh F. and Aubry, Marie-Pierre and Schmitz, Birger and Sherrell, Robert M.},
  issn         = {1872-616X},
  keyword      = {Paleocene/Eocene Thermal Maximum (PETM),Paleoproductivity,GSSP,section,Titanomagnetite,Magnetite,Chalcophile elements},
  language     = {eng},
  number       = {3-4},
  pages        = {365--377},
  publisher    = {Elsevier},
  series       = {Palaeogeography, Palaeoclimatology, Palaeoecology},
  title        = {Enhanced coastal paleoproductivity and nutrient supply in Upper Egypt during the Paleocene/Eocene Thermal Maximum (PETM): Mineralogical and geochemical evidence},
  url          = {http://dx.doi.org/10.1016/j.palaeo.2011.07.027},
  volume       = {310},
  year         = {2011},
}