[HTML][HTML] Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
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 …
Towards quantitative environmental reconstructions from ancient non-analogue microfossil assemblages: Ecological preferences of Paleocene–Eocene …
We explore a novel approach towards quantification of paleo-ecological signals from non-
analogue microfossil assemblages by quantifying relations between assemblages and high …
analogue microfossil assemblages by quantifying relations between assemblages and high …
Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum
Abstract The Palaeocene–Eocene Thermal Maximum (PETM) was a global warming event
of 5–6° C around 56 million years ago caused by input of carbon into the ocean and …
of 5–6° C around 56 million years ago caused by input of carbon into the ocean and …
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 …
Paleocene/Eocene carbon feedbacks triggered by volcanic activity
Abstract The Paleocene–Eocene Thermal Maximum (PETM) was a period of geologically-
rapid carbon release and global warming~ 56 million years ago. Although modelling …
rapid carbon release and global warming~ 56 million years ago. Although modelling …
[HTML][HTML] Effects of redox variability and early diagenesis on marine sedimentary Hg records
Volcanism is a dominant natural source of mercury (Hg) to the atmosphere, biosphere,
ocean and sediments. In recent years, sedimentary Hg contents have emerged as a tool to …
ocean and sediments. In recent years, sedimentary Hg contents have emerged as a tool to …
Global and zonal‐mean hydrological response to early Eocene warmth
Earth's hydrological cycle is expected to intensify in response to global warming, with a “wet‐
gets‐wetter, dry‐gets‐drier” response anticipated over the ocean. Subtropical regions (∼ …
gets‐wetter, dry‐gets‐drier” response anticipated over the ocean. Subtropical regions (∼ …
Lethal microbial blooms delayed freshwater ecosystem recovery following the end-Permian extinction
Harmful algal and bacterial blooms linked to deforestation, soil loss and global warming are
increasingly frequent in lakes and rivers. We demonstrate that climate changes and …
increasingly frequent in lakes and rivers. We demonstrate that climate changes and …
Arctic vegetation, temperature, and hydrology during Early Eocene transient global warming events
Early Eocene global climate was warmer than much of the Cenozoic and was punctuated by
a series of transient warming events or 'hyperthermals' associated with carbon isotope …
a series of transient warming events or 'hyperthermals' associated with carbon isotope …
Mercury anomalies across the Palaeocene–Eocene thermal maximum
Large-scale magmatic events like the emplacement of the North Atlantic Igneous Province
(NAIP) are often coincident with periods of extreme climate change such as the Palaeocene …
(NAIP) are often coincident with periods of extreme climate change such as the Palaeocene …