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Deconstructing the Lomagundi-Jatuli carbon isotope excursion
The early to mid-Paleoproterozoic Lomagundi-Jatuli Excursion (LJE) is ostensibly the
largest magnitude (approximately+ 5 to+ 30‰), longest duration (ca. 130–250 million years) …
largest magnitude (approximately+ 5 to+ 30‰), longest duration (ca. 130–250 million years) …
[HTML][HTML] Locating the BACE of the Cambrian: Bayan Gol in southwestern Mongolia and global correlation of the Ediacaran–Cambrian boundary
The diversification of animals during the Cambrian Period is one of the most significant
evolutionary events in Earth's history. However, the sequence of events leading to the origin …
evolutionary events in Earth's history. However, the sequence of events leading to the origin …
Modeling the impacts of diagenesis on carbonate paleoredox proxies
The geochemistry of the carbonate sedimentary record is invaluable for understanding the
ancient seawater evolution of carbon and redox-sensitive elements. However, the …
ancient seawater evolution of carbon and redox-sensitive elements. However, the …
Vertical decoupling in Late Ordovician anoxia due to reorganization of ocean circulation
Geochemical redox proxies indicate that seafloor anoxia occurred during the latest
Ordovician glacial maximum, coincident with the second pulse of the Late Ordovician mass …
Ordovician glacial maximum, coincident with the second pulse of the Late Ordovician mass …
The grandest of them all: the Lomagundi–Jatuli Event and Earth's oxygenation
The Paleoproterozoic Lomagundi–Jatuli Event (LJE) is generally considered the largest, in
both amplitude and duration, positive carbonate C-isotope (δ 13Ccarb) excursion in Earth …
both amplitude and duration, positive carbonate C-isotope (δ 13Ccarb) excursion in Earth …
The Ordovician of Scandinavia: a revised regional stage classification
Abstract The Ordovician of Scandinavia (ie Denmark, Norway and Sweden) has been
investigated for over two centuries and, through time, various chronostratigraphic schemes …
investigated for over two centuries and, through time, various chronostratigraphic schemes …
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] Sulfidic anoxia in the oceans during the Late Ordovician mass extinctions–insights from molybdenum and uranium isotopic global redox proxies
Abstract The Late Ordovician Mass Extinction wiped out 85% of animal species in two
phases (LOME1 and LOME2). The kill mechanisms for the extinction phases are debated …
phases (LOME1 and LOME2). The kill mechanisms for the extinction phases are debated …
Linking carbon cycle perturbations to the Late Ordovician glaciation and mass extinction: A modeling approach
Abstract The Hirnantian Stage of the Late Ordovician coincides with a positive carbon
isotope excursion (HICE,∼+ 6‰), a major glaciation, increased volcanic activity, expanded …
isotope excursion (HICE,∼+ 6‰), a major glaciation, increased volcanic activity, expanded …
A meta-analysis of the Steptoean positive carbon isotope excursion: the SPICEraq database
Abstract The Steptoean Positive Isotopic Carbon Excursion (SPICE) is a prominent
chemostratigraphic feature in the Lower Paleozoic. It has been used to correlate Upper …
chemostratigraphic feature in the Lower Paleozoic. It has been used to correlate Upper …