Methane feedbacks to the global climate system in a warmer world
Methane (CH4) is produced in many natural systems that are vulnerable to change under a
warming climate, yet current CH4 budgets, as well as future shifts in CH4 emissions, have …
warming climate, yet current CH4 budgets, as well as future shifts in CH4 emissions, have …
[HTML][HTML] Epochs, events and episodes: Marking the geological impact of humans
Event stratigraphy is used to help characterise the Anthropocene as a chronostratigraphic
concept, based on analogous deep-time events, for which we provide a novel …
concept, based on analogous deep-time events, for which we provide a novel …
Changing state of the climate system
2 Chapter 2 assesses observed large-scale changes in climate system drivers, key climate
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …
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 …
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 …
Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum
Abstract The Palaeocene–Eocene Thermal Maximum,(PETM) was a global warming event
that occurred about 56 million years ago, and is commonly thought to have been driven …
that occurred about 56 million years ago, and is commonly thought to have been driven …
[图书][B] Soils of the past: an introduction to paleopedology
GJ Retallack - 2008 - books.google.com
It has been 10 years since publication of the first edition ofSoils of the Past. In that time the
subject of paleopedology hasgrown rapidly, and established itself within the mainstream …
subject of paleopedology hasgrown rapidly, and established itself within the mainstream …
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 …
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 …
The seawater carbon inventory at the Paleocene–Eocene Thermal Maximum
The Paleocene–Eocene Thermal Maximum (PETM)(55.6 Mya) was a geologically rapid
carbon-release event that is considered the closest natural analog to anthropogenic CO2 …
carbon-release event that is considered the closest natural analog to anthropogenic CO2 …