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 …
Abstract The Permian–Triassic mass extinction was marked by a massive release of carbon into the ocean-atmosphere system, evidenced by a sharp negative carbon isotope …
W Ruebsam, M Reolid, N Sabatino, D Masetti… - Global and Planetary …, 2020 - Elsevier
In this paper, we use molecular paleothermometry, based on the TEX 86 proxy derived from fossilized archaeal lipids, to reconstruct absolute sea surface temperatures (SSTs) for the …
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 …
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 …
Abstract The Toarcian Oceanic Anoxic Event (T-OAE,∼ 183 Ma) was marked by a pronounced negative carbon-isotope excursion, rapid global warming, ocean …
Abstract The early Toarcian (Early Jurassic) Oceanic Anoxic Event (T-OAE) or Jenkyns Event (~ 183 Ma) was marked by a globally synchronous negative carbon-isotope …
Abstract The Early Jurassic Jenkyns Event (∼ 183 Ma) was characterized in terrestrial environments by global warming, perturbation of the carbon cycle, enhanced weathering …
W Ruebsam, M Al-Husseini - Gondwana Research, 2020 - Elsevier
Abstract Cyclostratigraphic analyses of Upper Pliensbachian and Lower Toarcian carbon-13 isotope (δ 13 C) data, together with radiometric dating, are used to calibrate biozones and …