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Global organic carbon burial during the Toarcian oceanic anoxic event: Patterns and controls
The early Toarcian oceanic anoxic event (T-OAE,~ 183 Ma), also known as the Jenkyns
Event, was one of the most important hyperthermal events of the Phanerozoic, caused by the …
Event, was one of the most important hyperthermal events of the Phanerozoic, caused by the …
Oceanic anoxic events, photic-zone euxinia, and controversy of sea-level fluctuations during the Middle-Late Devonian
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 …
Mississippian, as well as the possible triggers and controls of these events. These “anoxic …
Terrestrial sources as the primary delivery mechanism of mercury to the oceans across the Toarcian Oceanic Anoxic Event (Early Jurassic)
This study evaluates the utility of sedimentary mercury (Hg) contents as a proxy for
fingerprinting ancient massive volcanism, which is often associated with biogeochemical …
fingerprinting ancient massive volcanism, which is often associated with biogeochemical …
Carbon-cycle changes during the Toarcian (Early Jurassic) and implications for regional versus global drivers of the Toarcian oceanic anoxic event
Abstract The Early Jurassic Toarcian oceanic anoxic event (T-OAE) is characterized by an
extinction event, a major sea-level rise, enhanced marine primary productivity, elevated …
extinction event, a major sea-level rise, enhanced marine primary productivity, elevated …
The Triassic–Jurassic transition–A review of environmental change at the dawn of modern life
Abstract The Triassic–Jurassic transition, which is here broadly defined as extending from
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
Two types of hyperthermal events in the Mesozoic-Cenozoic: Environmental impacts, biotic effects, and driving mechanisms
A deeper understanding of hyperthermal events in the Earth's history can provide an
important scientific basis for understanding and co** with global warming in the …
important scientific basis for understanding and co** with global warming in the …
The Toarcian oceanic anoxic event in southwestern Gondwana: an example from the Andean Basin, northern Chile
A Fantasia, KB Föllmi, T Adatte… - Journal of the …, 2018 - lyellcollection.org
Palaeoenvironmental and palaeoclimatic changes during the Toarcian Oceanic Anoxic
Event (T-OAE) are reported from two successions deposited in the Andean Basin (Chile) …
Event (T-OAE) are reported from two successions deposited in the Andean Basin (Chile) …
Carbonate uranium isotopes record global expansion of marine anoxia during the Toarcian Oceanic Anoxic Event
The Toarcian Oceanic Anoxic Event (T-OAE;~ 183 Mya) was a globally significant carbon-
cycle perturbation linked to widespread deposition of organic-rich sediments, massive …
cycle perturbation linked to widespread deposition of organic-rich sediments, massive …
Elevated atmospheric CO2 drove an increase in tropical cyclone intensity during the early Toarcian hyperthermal
The occurrence of sedimentary storm deposits around the Tethys Ocean during the early
Toarcian hyperthermal (~ 183 Ma) suggests that intensified tropical cyclone (TC) activity …
Toarcian hyperthermal (~ 183 Ma) suggests that intensified tropical cyclone (TC) activity …
Two-phased collapse of the shallow-water carbonate factory during the late Pliensbachian–Toarcian driven by changing climate and enhanced continental …
Abstract The end Pliensbachian–Toarcian is characterized by several carbon-cycle
perturbations and faunal turnovers (eg, ammonites and foraminifera), which are most likely …
perturbations and faunal turnovers (eg, ammonites and foraminifera), which are most likely …