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 …

This paper reviews global records of anoxic events of the Middle Devonian–earliest
Mississippian, as well as the possible triggers and controls of these events. These “anoxic …

A long-term record of global mean surface temperature (GMST) provides critical insight into
the dynamical limits of Earth's climate and the complex feedbacks between temperature and …

Atmospheric CO2 is thought to play a fundamental role in Earth's climate regulation. Yet, for
much of Earth's geological past, atmospheric CO2 has been poorly constrained, hindering …

Orbital forcing affects climate system by regulating the amount of solar radiation received at
the Earth's surface, which is vital for global hydrological cycles. However, a systematic …

Three intervals of glaciomarine diamictites with extensive glendonites in middle to upper
Permian sediments were found in the Kobyume River, southern Verkhoyanie, Russia. The …

The late Paleozoic ice age (LPIA) was the longest-lived glaciation of the Phanerozoic, and
the demise of LPIA is the Earth's only recorded transition from an icehouse to a greenhouse …

For more than 150 years, geologic characteristics claimed to be evidence for pre-
Pleistocene glaciations have been debated. Advancements in recent decades, in …

The late Paleozoic glacial-to-postglacial turnover evolved complexly across Gondwana.
Successions bearing volcaniclastic material that can be radiometrically dated provide crucial …

Abstract The Late Paleozoic Ice Age (LPIA) was the longest and most extensive glacial
interval during the Phanerozoic, lasting from the Late Devonian to the late Permian (362 …