[HTML][HTML] Long-term Phanerozoic global mean sea level: Insights from strontium isotope variations and estimates of continental glaciation

DG van der Meer, CR Scotese, BJW Mills, A Sluijs… - Gondwana …, 2022 - Elsevier
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 …

Steep oceanic DIC δ13C depth gradient during the Hirnantian Glaciation

S Yang, J Fan, TJ Algeo, GA Shields, Y Zhou, C Li… - Earth-Science …, 2024 - Elsevier
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 …

[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 …

The PhanSST global database of Phanerozoic sea surface temperature proxy data

EJ Judd, JE Tierney, BT Huber, SL Wing, DJ Lunt… - Scientific Data, 2022 - nature.com
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 …

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 …

Osmium and lithium isotope evidence for weathering feedbacks linked to orbitally paced organic carbon burial and Silurian glaciations

AD Sproson, PAEP von Strandmann, D Selby… - Earth and Planetary …, 2022 - Elsevier
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 …

Marine anoxia as a trigger for the largest Phanerozoic positive carbon isotope excursion: Evidence from carbonate barium isotope record

F Zhang, J Frýda, M Fakhraee, Y Lin, GY Wei… - Earth and Planetary …, 2022 - Elsevier
Abstract The mid-Ludfordian Lau carbon isotope excursion (Lau CIE) represents the largest
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 …

K Thue, LA Buatois, MG Mángano, M Ornia - Sedimentary Geology, 2024 - Elsevier
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 …

[HTML][HTML] Dynamics of Silurian plants as response to climate changes

J Pšenička, J Bek, J Frýda, V Žárský, M Uhlířová… - Life, 2021 - mdpi.com
The most ancient macroscopic plants fossils are Early Silurian cooksonioid sporophytes
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 …