The early Toarcian Oceanic Anoxic Event (Jenkyns Event) in the Alpine-Mediterranean Tethys, north African margin, and north European epicontinental seaway
Abstract The early Toarcian Oceanic Anoxic Event (Jenkyns Event) was associated with
major world-wide climatic changes with profound effects on the global carbon cycle. This …
major world-wide climatic changes with profound effects on the global carbon cycle. This …
[HTML][HTML] An Early Jurassic (Sinemurian–Toarcian) stratigraphic framework for the occurrence of organic matter preservation intervals (OMPIs)
Lower Jurassic sedimentary successions in the Atlantic margin basins include several
organic-rich intervals, some with source rock potential; time-equivalent units are also …
organic-rich intervals, some with source rock potential; time-equivalent units are also …
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 …
Reduced plate motion controlled timing of Early Jurassic Karoo-Ferrar large igneous province volcanism
Past large igneous province (LIP) emplacement is commonly associated with mantle plume
upwelling and led to major carbon emissions. One of Earth's largest past environmental …
upwelling and led to major carbon emissions. One of Earth's largest past environmental …
Mercury sequestration pathways under varying depositional conditions during Early Jurassic (Pliensbachian and Toarcian) Karoo-Ferrar volcanism
Major extinction events appear coincident with the emplacement of large igneous provinces
(LIPs) throughout Earth's past, but the cause-and-effect relationship is often poorly …
(LIPs) throughout Earth's past, but the cause-and-effect relationship is often poorly …
The Toarcian Oceanic Anoxic Event: where do we stand?
The study of past climate changes is pivotal for understanding the complex biogeochemical
interactions through time between the geosphere, atmosphere, hydrosphere and biosphere …
interactions through time between the geosphere, atmosphere, hydrosphere and biosphere …
Ecosystem recovery after the Early Jurassic T-OAE in the Châabet El Attaris section of the Tunisian Atlas
M Reolid, M Soussi, W Ruebsam, IBH Taher… - Palaeogeography …, 2023 - Elsevier
The flooding of the Pliensbachian shelf of the North-South Axis of Central Tunisia during the
early Toarcian favoured the development of organic-rich facies in the most subsiding areas …
early Toarcian favoured the development of organic-rich facies in the most subsiding areas …
[HTML][HTML] Orbitally synchronized late Pliensbachian–early Toarcian glacio-eustatic and carbon-isotope cycles
W Ruebsam, M Al-Husseini - Palaeogeography, Palaeoclimatology …, 2021 - Elsevier
Abstract The late Pliensbachian–early Toarcian δ 13 C org in the Mochras Core (UK)
consists of segments (rising and falling limbs, valleys, plateaus) that correlate to coeval …
consists of segments (rising and falling limbs, valleys, plateaus) that correlate to coeval …
Primary v. carbonate production in the Toarcian, a case study from the Llanbedr (Mochras Farm) borehole, Wales
The leading hypothesis for the Toarcian oceanic anoxic event (T-OAE; c. 183 Ma) and the
associated negative C-isotope excursion is the massive release of 12 C favouring …
associated negative C-isotope excursion is the massive release of 12 C favouring …
Suboxic conditions prevailed during the Toarcian Oceanic Anoxic Event in the Alpine-Mediterranean Tethys: The Sogno Core pelagic record (Lombardy Basin …
Abstract The Sogno Core represents one of the deepest pelagic records of the Toarcian
Oceanic Anoxic Event (T-OAE) in the Alpine-Mediterranean Tethys. New sedimentological …
Oceanic Anoxic Event (T-OAE) in the Alpine-Mediterranean Tethys. New sedimentological …