Milankovitch cycles are quasi-periodic fluctuations in insolation forced by the variation in
Earth's astronomical parameters. The astronomically induced climate change affected the …

Astronomical insolation forcing is well established as the underlying metronome of
Quaternary ice ages and Cenozoic climate changes. Yet its effects on earlier eras …

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 …

Abstract The Ordovician of Scandinavia (ie Denmark, Norway and Sweden) has been
investigated for over two centuries and, through time, various chronostratigraphic schemes …

The sedimentological and geochemical expression of Mesozoic ocean anoxic events
(OAEs) in the geologic record is reasonably well-characterized and the causal mechanisms …

Abstract The Late Devonian biodiversity crisis, one of the big five Phanerozoic diversity
depletions, is composed of a series of extinction events broadly coincident with the invasion …

The evolution and expansion of land plants brought about one of the most dramatic shifts in
the history of the Earth system—the birth of modern soils—and likely stimulated massive …

The use of portable Energy Dispersive X-Ray Fluorescence (pXRF) spectrometers has
exploded within the last decade for eg, environmental, geological, and archaeological field …

Oceanic anoxia is considered as the immediate cause of the Frasnian–Famennian mass
extinction, yet the frequency of anoxia and associated environmental modulators remains …

We present comprehensive Li-C-Sr isotopic studies on two classic marine carbonate
sections (Yangdi and Dongcun) transecting the Late Devonian Frasnian-Famennian …