Turnitin
降AI改写
早检测系统
早降重系统
Turnitin-UK版
万方检测-期刊版
维普编辑部版
Grammarly检测
Paperpass检测
checkpass检测
PaperYY检测
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 …
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 1, 2 (PETM) was a global warming
event that occurred about 56 million years ago, and is commonly thought to have been …
event that occurred about 56 million years ago, and is commonly thought to have been …
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 …
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 …
Tracing North Atlantic volcanism and seaway connectivity across the paleocene–eocene thermal maximum (PETM)
There is a temporal correlation between the peak activity of the North Atlantic Igneous
Province (NAIP) and the Paleocene–Eocene Thermal Maximum (PETM), suggesting that the …
Province (NAIP) and the Paleocene–Eocene Thermal Maximum (PETM), suggesting that the …
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 …
Loss of Earth system resilience during early Eocene transient global warming events
Superimposed on long-term late Paleocene–early Eocene warming (~ 59 to 52 million years
ago), Earth's climate experienced a series of abrupt perturbations, characterized by massive …
ago), Earth's climate experienced a series of abrupt perturbations, characterized by massive …