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[HTML][HTML] Long-term Phanerozoic global mean sea level: Insights from strontium isotope variations and estimates of continental glaciation
Global mean sea level is a key component within the fields of climate and oceanographic
modelling in the Anthropocene. Hence, an improved understanding of eustatic sea level in …
modelling in the Anthropocene. Hence, an improved understanding of eustatic sea level in …
Steep oceanic DIC δ13C depth gradient during the Hirnantian Glaciation
The Hirnantian carbon isotopic excursion (HICE) was characterized by a positive δ 13 C
excursion (up to~+ 7‰) of oceanic dissolved inorganic carbon (DIC). However its …
excursion (up to~+ 7‰) of oceanic dissolved inorganic carbon (DIC). However its …
[HTML][HTML] Silurian wildfire proxies and atmospheric oxygen
IJ Glasspool, RA Gastaldo - Geology, 2022 - pubs.geoscienceworld.org
The earliest evidence of wildfire is documented from two localities: the early mid-Silurian
Pen-y-lan Mudstone, Rumney, Wales (UK), and the late Silurian Winnica Formation …
Pen-y-lan Mudstone, Rumney, Wales (UK), and the late Silurian Winnica Formation …
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 …
Chemical–to–reverse weathering triggered a pronounced positive carbon isotope excursion in a forced regressive to transgressive dolostone succession during the …
Y Zhang, G Zhu, X Li, Y Ai, P Duan, M Li… - Global and Planetary …, 2024 - Elsevier
Abstract The terminal Ediacaran (∼ 551–541 Ma) was a critical period in Earth's history
witnessing the coupled evolution of tectonism, climate, marine environment, and …
witnessing the coupled evolution of tectonism, climate, marine environment, and …
Osmium and lithium isotope evidence for weathering feedbacks linked to orbitally paced organic carbon burial and Silurian glaciations
Abstract The Ordovician (∼ 487 to 443 Ma) ended with the formation of extensive Southern
Hemisphere ice sheets, known as the Hirnantian glaciation, and the second largest mass …
Hemisphere ice sheets, known as the Hirnantian glaciation, and the second largest mass …
Marine anoxia as a trigger for the largest Phanerozoic positive carbon isotope excursion: Evidence from carbonate barium isotope record
Abstract The mid-Ludfordian Lau carbon isotope excursion (Lau CIE) represents the largest
positive carbon isotope excursion in the Phanerozoic (∼ 9‰), coincident with the …
positive carbon isotope excursion in the Phanerozoic (∼ 9‰), coincident with the …
[HTML][HTML] Benthic response to event deposition and environmental disturbance in a shoreface to subaqueous delta system: Ichnology of the Silurian-Devonian Furada …
Abstract The Furada Formation of Asturias, Spain, represents a clastic shallow-marine unit
deposited during the middle Silurian to the Early Devonian. This formation contains …
deposited during the middle Silurian to the Early Devonian. This formation contains …
[HTML][HTML] Dynamics of Silurian plants as response to climate changes
The most ancient macroscopic plants fossils are Early Silurian cooksonioid sporophytes
from the volcanic islands of the peri-Gondwanan palaeoregion (the Barrandian area, Prague …
from the volcanic islands of the peri-Gondwanan palaeoregion (the Barrandian area, Prague …
Carbon and conodont apatite oxygen isotope records from the Alengchu section in western Yunnan and their paleoclimatic and paleogeographic implications
B Chen, MQ Zhang, WK Qie, K Liang, JF Lu… - Palaeoworld, 2024 - Elsevier
Abstract The Early Devonian witnessed dramatic changes in climate, ocean chemistry and
faunal evolution. However, previous studies have relied mainly on records from North …
faunal evolution. However, previous studies have relied mainly on records from North …