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Basalt‐seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: deconstructing Oceanic Anoxic Event 2 (Cenomanian–Turonian …
Abstract Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major
palaeoceanographic phenomenon that took place during an interval of extreme global …
palaeoceanographic phenomenon that took place during an interval of extreme global …
[HTML][HTML] Exploring the paleoceanographic changes registered by planktonic foraminifera across the Cenomanian-Turonian boundary interval and Oceanic Anoxic …
MR Petrizzo, DK Watkins, KG MacLeod… - Global and Planetary …, 2021 - Elsevier
Planktonic foraminiferal population dynamics and benthic foraminiferal and radiolaria
distributions combined with δ 13 C and δ 18 O measurements of both bulk carbonate and …
distributions combined with δ 13 C and δ 18 O measurements of both bulk carbonate and …
A Re‐evaluation of the Plenus Cold Event, and the Links Between CO2, Temperature, and Seawater Chemistry During OAE 2
The greenhouse world of the mid‐Cretaceous (~ 94 Ma) was punctuated by an episode of
abrupt climatic upheaval: Oceanic Anoxic Event 2. High‐resolution climate records reveal …
abrupt climatic upheaval: Oceanic Anoxic Event 2. High‐resolution climate records reveal …
High-resolution records of Oceanic Anoxic Event 2: Insights into the timing, duration and extent of environmental perturbations from the palaeo-South Pacific Ocean
Abstract Oceanic Anoxic Event 2 (OAE 2), which took place around the Cenomanian–
Turonian boundary (∼ 94 Ma), is associated with extreme perturbations to the global carbon …
Turonian boundary (∼ 94 Ma), is associated with extreme perturbations to the global carbon …
High-resolution bio-and chemostratigraphy of an expanded record of Oceanic Anoxic Event 2 (late Cenomanian–early Turonian) at Clot Chevalier, near Barrême, SE …
A newly located exposure of the Niveau Thomel, an organic-rich level at the Cenomanian–
Tur-onian boundary, provides a highly expanded record of Oceanic Anoxic Event (OAE) 2 …
Tur-onian boundary, provides a highly expanded record of Oceanic Anoxic Event (OAE) 2 …
[HTML][HTML] Benthic foraminiferal response to the Oceanic Anoxic Event 2 (Late Cretaceous) and evidence of bottom water re‐oxygenation during the Plenus Cold Event …
Abstract The Cenomanian-Turonian boundary interval is characterized by environmental
perturbations related to the Oceanic Anoxic Event 2 (OAE 2) that severely affected the …
perturbations related to the Oceanic Anoxic Event 2 (OAE 2) that severely affected the …
Organic matter geochemistry and petrography of Late Cretaceous (Cenomanian-Turonian) organic-rich shales from the Belle Fourche and Second White Specks …
Organic-rich mudstones with up to 10 wt% TOC from the upper portion of the Belle Fourche
Formation and the lower part of the Second White Specks Formation in the Western Canada …
Formation and the lower part of the Second White Specks Formation in the Western Canada …
The Cenomanian–Turonian transition in the carbonate platform facies of the Western Saharan Atlas (Rhoundjaïa formation, Algeria)
Microfacies, fossil macroinvertebrates and microfossil assemblages (foraminifera and
ostracods) and δ 13 C from the Rhoundjaïa Formation (Ksour Mountains, Western Saharan …
ostracods) and δ 13 C from the Rhoundjaïa Formation (Ksour Mountains, Western Saharan …
The giant inoceramid Platyceramus platinus as a high-resolution paleoclimate archive for the Late Cretaceous of the Western Interior Seaway
EO Walliser, R Mertz-Kraus, BR Schöne - Cretaceous Research, 2018 - Elsevier
Platyceramus platinus was a giant inoceramid bivalve that inhabited the outer shelf
environments of the Western Interior Seaway (WIS) in North America. With axial heights …
environments of the Western Interior Seaway (WIS) in North America. With axial heights …
Organic petrography and geochemical characterization of the Upper Cretaceous Second White Specks and Upper Belle Fourche alloformations, west-central Alberta …
MA Aviles, OH Ardakani, BA Cheadle… - International Journal of …, 2019 - Elsevier
Abstract The Second White Specks is an enigmatic unconventional shale play in the
Western Canada Foreland Basin (WCFB). This play has an inconsistent production …
Western Canada Foreland Basin (WCFB). This play has an inconsistent production …