Phanerozoic paleotemperatures: The earth's changing climate during the last 540 million years
This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …
have changed during the last 540 million years. It combines paleotemperature …
A revised, late Palaeozoic glacial time-space framework for eastern Australia, and comparisons with other regions and events
A timeframe of glacial and nonglacial intervals in the Carboniferous and Permian systems of
eastern Australia was published by Fielding et al.(2008a). In this scheme, eight discrete …
eastern Australia was published by Fielding et al.(2008a). In this scheme, eight discrete …
Age and pattern of the southern high-latitude continental end-Permian extinction constrained by multiproxy analysis
Past studies of the end-Permian extinction (EPE), the largest biotic crisis of the Phanerozoic,
have not resolved the timing of events in southern high-latitudes. Here we use palynology …
have not resolved the timing of events in southern high-latitudes. Here we use palynology …
End-Permian (252 Mya) deforestation, wildfires and flooding—an ancient biotic crisis with lessons for the present
Current large-scale deforestation poses a threat to ecosystems globally, and imposes
substantial and prolonged changes on the hydrological and carbon cycles. The tropical …
substantial and prolonged changes on the hydrological and carbon cycles. The tropical …
Evaluation of physical and chemical proxies used to interpret past glaciations with a focus on the late Paleozoic Ice Age
Abstract The late Paleozoic Ice Age (LPIA) was one of Earth's most important Phanerozoic
climatic events lasting for over 100 Mys. Despite its importance, its history is controversial …
climatic events lasting for over 100 Mys. Despite its importance, its history is controversial …
High-resolution SIMS oxygen isotope analysis on conodont apatite from South China and implications for the end-Permian mass extinction
Understanding the interplay of climatic and biological events in deep time requires resolving
the precise timing and pattern of paleotemperature changes and their temporal relationship …
the precise timing and pattern of paleotemperature changes and their temporal relationship …
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 …
Age constraints of the glaciation in the Paraná Basin: evidence from new U–Pb dates
The absence of absolute dating in glacial deposits of the Paraná Basin prevents better
understanding of the complete history of the Late Palaeozoic Ice Age in Western Gondwana …
understanding of the complete history of the Late Palaeozoic Ice Age in Western Gondwana …
Early Wuchiapingian cooling linked to Emeishan basaltic weathering?
The last glaciation during the late Paleozoic ice age commenced at around the Guadalupian–
Lopingian (G–L) boundary and is synchronous with the emplacement of the Emeishan large …
Lopingian (G–L) boundary and is synchronous with the emplacement of the Emeishan large …
The chemical index of alteration in Permo-Carboniferous strata in North China as an indicator of environmental and climate change throughout the late Paleozoic Ice …
Y Li, L Shao, CR Fielding, TD Frank, D Wang… - Global and Planetary …, 2023 - Elsevier
Abstract Comparison of chemical index of alteration (CIA) values and estimated land surface
temperatures (LSTs) from upper Carboniferous-Permian successions in low paleolatitude …
temperatures (LSTs) from upper Carboniferous-Permian successions in low paleolatitude …