[HTML][HTML] Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
MJ Carmichael, GN Inglis, MPS Badger… - Global and Planetary …, 2017 - Elsevier
Abstract The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal,~ 56 million years
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …
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 …
How Large Igneous Provinces affect global climate, sometimes cause mass extinctions, and represent natural markers in the geological record
Abstract Large Igneous Provinces (LIPs) can have a significant global climatic effect as
monitored by sedimentary trace and isotopic compositions that record paleo …
monitored by sedimentary trace and isotopic compositions that record paleo …
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 …
Mercury evidence for pulsed volcanism during the end-Triassic mass extinction
The Central Atlantic Magmatic Province (CAMP) has long been proposed as having a
causal relationship with the end-Triassic extinction event (∼ 201.5 Ma). In North America …
causal relationship with the end-Triassic extinction event (∼ 201.5 Ma). In North America …
Cryosphere carbon dynamics control early Toarcian global warming and sea level evolution
The Earth's cryosphere represents a huge climate-sensitive carbon reservoir capable of
releasing carbon dioxide (CO 2) and methane (CH 4) from permafrost soils or gas reservoirs …
releasing carbon dioxide (CO 2) and methane (CH 4) from permafrost soils or gas reservoirs …
Carbon sequestration in an expanded lake system during the Toarcian oceanic anoxic event
Abstract The Early Jurassic Toarcian oceanic anoxic event (∼ 183 Ma) was marked by
marine anoxia–euxinia and globally significant organic-matter burial, accompanied by a …
marine anoxia–euxinia and globally significant organic-matter burial, accompanied by a …
Orbital pacing and secular evolution of the Early Jurassic carbon cycle
Global perturbations to the Early Jurassic environment (∼ 201 to∼ 174 Ma), notably during
the Triassic–Jurassic transition and Toarcian Oceanic Anoxic Event, are well studied and …
the Triassic–Jurassic transition and Toarcian Oceanic Anoxic Event, are well studied and …
[PDF][PDF] Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other …
Mercury (Hg) is increasingly being used as a sedimentary tracer of Large Igneous Province
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …
The Jurassic Period
Ammonites underwent an evolutionary diversification after the mass extinction of the end
Triassic induced by the formation of a Large Igneous province (LIP), and this group provides …
Triassic induced by the formation of a Large Igneous province (LIP), and this group provides …