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On impact and volcanism across the Cretaceous-Paleogene boundary
The cause of the end-Cretaceous mass extinction is vigorously debated, owing to the
occurrence of a very large bolide impact and flood basalt volcanism near the boundary …
occurrence of a very large bolide impact and flood basalt volcanism near the boundary …
Terrestrial climate in mid-latitude East Asia from the latest Cretaceous to the earliest Paleogene: A multiproxy record from the Songliao Basin in northeastern China
From the latest Cretaceous (late Campanian to Maastrichtian,~ 75–66 Ma) to the earliest
Paleogene, fluctuations in greenhouse climate, inferred primarily from marine sediments …
Paleogene, fluctuations in greenhouse climate, inferred primarily from marine sediments …
A high‐Fidelity benthic stable isotope record of late Cretaceous–early Eocene climate change and carbon‐cycling
Abstract The Late Cretaceous–Early Paleogene is the most recent period in Earth history
that experienced sustained global greenhouse warmth on multimillion year timescales. Yet …
that experienced sustained global greenhouse warmth on multimillion year timescales. Yet …
[PDF][PDF] Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other …
Mercury (Hg) is increasingly being used as a sedimentary tracer of Large Igneous Province
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …
Maastrichtian to Danian Atlantic transgression in the north of Patagonia: a dinoflagellate cyst approach
MV Guler, MSG Estebenet, EL Navarro… - Journal of South …, 2019 - Elsevier
The late Maastrichtian to early Paleocene marine successions in northern Patagonia and
neighboring southwestern Atlantic Ocean Basins provided a valuable organic-walled …
neighboring southwestern Atlantic Ocean Basins provided a valuable organic-walled …
[HTML][HTML] A new high-resolution chronology for the late Maastrichtian warming event: Establishing robust temporal links with the onset of Deccan volcanism
The late Maastrichtian warming event was defined by a global temperature increase of∼ 2.5–
5 C that occurred∼ 150–300 ky before the Cretaceous-Paleogene (K-Pg) mass extinction …
5 C that occurred∼ 150–300 ky before the Cretaceous-Paleogene (K-Pg) mass extinction …
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 …
Contribution of orbital forcing and Deccan volcanism to global climatic and biotic changes across the Cretaceous-Paleogene boundary at Zumaia, Spain
Untangling the timing of the environmental effects of Deccan volcanism with respect to the
Chicxulub impact is instrumental to fully assessing the contributions of both to climate …
Chicxulub impact is instrumental to fully assessing the contributions of both to climate …
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 …
[KNIHA][B] Mesozoic mammals from South America and their forerunners
GW Rougier, AG Martinelli, AM Forasiepi - 2021 - Springer
As evolutionary biologists, we live in exciting and promising times. The material basis of our
science is growing at an unprecedented rate; fossils preserving structures we thought …
science is growing at an unprecedented rate; fossils preserving structures we thought …