The Paleocene-Eocene benthic foraminiferal extinction and stable isotope anomalies
E Thomas, NJ Shackleton - Geological Society, London, Special …, 1996 - lyellcollection.org
In the late Paleocene to early Eocene, deep sea benthic foraminifera suffered their only
global extinction of the last 75 million years and diversity decreased worldwide by 30–50 …
global extinction of the last 75 million years and diversity decreased worldwide by 30–50 …
Coupled greenhouse warming and deep‐sea acidification in the middle Eocene
The Middle Eocene Climatic Optimum (MECO) is an enigmatic warming event that
represents an abrupt reversal in long‐term cooling through the Eocene. In order to further …
represents an abrupt reversal in long‐term cooling through the Eocene. In order to further …
Eocene global warming events driven by ventilation of oceanic dissolved organic carbon
Abstract 'Hyperthermals' are intervals of rapid, pronounced global warming known from six
episodes within the Palaeocene and Eocene epochs (∼ 65–34 million years (Myr) …
episodes within the Palaeocene and Eocene epochs (∼ 65–34 million years (Myr) …
[PDF][PDF] Explanatory notes
SS Party - Curry, WB, Shackleton, NJ, Richter, C., et al., Proc …, 1995 - primarydocuments.ca
•.. 4 (l) No proclat: wte. ion abal. li•• u• under••• e~ ion 1 before the expiry o! one yeAr from
the date of ehe passage ot the resolution in1tiat1n; the amen4ment procedure, unleae the …
the date of ehe passage ot the resolution in1tiat1n; the amen4ment procedure, unleae the …
Radwany Formation: A new formation name for the Early-Middle Eocene carbonate sediments of the offshore October oil field, Gulf of Suez: Contribution to the Eocene …
The Eocene sediments plays critical role in the evolution and development of the petroleum
system in the Gulf of Suez region, where it is representing a self-source rock or self-reservoir …
system in the Gulf of Suez region, where it is representing a self-source rock or self-reservoir …
Benthic foraminiferal assemblages from the eastern Weddell Sea between 68 and 73 S: Distribution, ecology and fossilization potential
A Mackensen, H Grobe, G Kuhn, DK Fu - Marine micropaleontology, 1990 - Elsevier
Surface sediment samples taken with a vented☐ corer from the eastern Weddell Sea on four
profiles perpendicular to the continental margin have been investigated for their benthic …
profiles perpendicular to the continental margin have been investigated for their benthic …
A benthic foraminiferal record of Paleocene sea level and trophic/redox conditions at Gebel Aweina, Egypt
RP Speijer, B Schmitz - Palaeogeography, Palaeoclimatology …, 1998 - Elsevier
We quantitatively analyzed benthic foraminiferal assemblages in order to reveal biotic and
paleoenvironmental trends in the Paleocene section of Gebel Aweina, Egypt, on the …
paleoenvironmental trends in the Paleocene section of Gebel Aweina, Egypt, on the …
Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35 and 57 S: Distribution, ecology and fossilization potential
Surface sediment samples taken with a multiple corer from the Polar Front region along two
profiles in the eastern South Atlantic sector between 35° and 57° S have been investigated …
profiles in the eastern South Atlantic sector between 35° and 57° S have been investigated …
The Late Campanian and Maastrichtian in northwestern Tunisia: palaeoenvironmental inferences from lithology, macrofauna and benthic foraminifera
L Li, G Keller, W Stinnesbeck - Cretaceous Research, 1999 - Elsevier
Late Campanian through Maastrichtian sea-level changes are examined based on lithology,
macrofossils and benthic foraminifera at the Elles and El Kef sections in Tunisia. Six major …
macrofossils and benthic foraminifera at the Elles and El Kef sections in Tunisia. Six major …
Development of the southern Eastern Cordillera, NW Argentina, constrained by apatite fission track thermochronology: From early Cretaceous extension to middle …
For the Puna Plateau and Eastern Cordillera of NW Argentina, the temporal and spatial
pattern of deformation and surface uplift remain poorly constrained. Analysis of completely …
pattern of deformation and surface uplift remain poorly constrained. Analysis of completely …