[HTML][HTML] Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes
It is well established that greenhouse conditions prevailed during the Cretaceous Period (~
145–66 Ma). Determining the exact nature of the greenhouse-gas forcing, climatic warming …
145–66 Ma). Determining the exact nature of the greenhouse-gas forcing, climatic warming …
Quantifying the pattern of organic carbon burial through Cretaceous Oceanic Anoxic Event 2
Abstract The Cenomanian-Turonian Oceanic Anoxic Event 2 (OAE 2, ca. 94 Ma) is
characterized by a marked positive carbon isotope excursion (CIE) recorded in global …
characterized by a marked positive carbon isotope excursion (CIE) recorded in global …
Archaeal lipids trace ecology and evolution of marine ammonia-oxidizing archaea
R Rattanasriampaipong, YG Zhang… - Proceedings of the …, 2022 - National Acad Sciences
Archaeal membrane lipids are widely used for paleotemperature reconstructions, yet these
molecular fossils also bear rich information about ecology and evolution of marine ammonia …
molecular fossils also bear rich information about ecology and evolution of marine ammonia …
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 …
The PhanSST global database of Phanerozoic sea surface temperature proxy data
Paleotemperature proxy data form the cornerstone of paleoclimate research and are integral
to understanding the evolution of the Earth system across the Phanerozoic Eon. Here, we …
to understanding the evolution of the Earth system across the Phanerozoic Eon. Here, we …
An early Cambrian greenhouse climate
The oceans of the early Cambrian (~ 541 to 509 million years ago) were the setting for a
marked diversification of animal life. However, sea temperatures—a key component of the …
marked diversification of animal life. However, sea temperatures—a key component of the …
Origin of limestone–marlstone cycles: astronomic forcing of organic-rich sedimentary rocks from the Cenomanian to early Coniacian of the Cretaceous Western Interior …
We present an integrated multidisciplinary study of limestone–marlstone couplets from a
continuously cored section including parts of the upper Buda Limestone, the entire Eagle …
continuously cored section including parts of the upper Buda Limestone, the entire Eagle …
Cretaceous large igneous provinces: from volcanic formation to environmental catastrophes and biological crises
Abstract The Cretaceous Period was marked by the formation of numerous large igneous
provinces (LIPs), several of which were associated with geologically rapid climate …
provinces (LIPs), several of which were associated with geologically rapid climate …
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 …
Chronostratigraphic framework and depositional environments in the organic‐rich, mudstone‐dominated Eagle Ford Group, Texas, USA
Since the beginning of the century, several authors have hypothesized and documented the
presence of bottom currents during the deposition of mudstones, including mudstones rich in …
presence of bottom currents during the deposition of mudstones, including mudstones rich in …