Silicate weathering as a feedback and forcing in Earth's climate and carbon cycle
Current understanding of the long-term carbon cycle posits that Earth's climate is stabilized
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …
The first large-scale bioavailable Sr isotope map of China and its implication for provenance studies
Abstract Strontium isotope ratio (87 Sr/86 Sr) has been widely used to trace human
migrations across geologically distinct landscapes in archaeological and forensic sciences …
migrations across geologically distinct landscapes in archaeological and forensic sciences …
How temperature-dependent silicate weathering acts as Earth's geological thermostat
SL Brantley, A Shaughnessy, MI Lebedeva… - Science, 2023 - science.org
Earth's climate may be stabilized over millennia by solubilization of atmospheric carbon
dioxide (CO2) as minerals weather, but the temperature sensitivity of this thermostat is …
dioxide (CO2) as minerals weather, but the temperature sensitivity of this thermostat is …
High‐resolution map** of the global silicate weathering carbon sink and its long‐term changes
C Li, X Bai, Q Tan, G Luo, L Wu, F Chen… - Global Change …, 2022 - Wiley Online Library
Climatic and non‐climatic factors affect the chemical weathering of silicate rocks, which in
turn affects the CO2 concentration in the atmosphere on a long‐term scale. However, the …
turn affects the CO2 concentration in the atmosphere on a long‐term scale. However, the …
Effects of carbonate minerals and exogenous acids on carbon flux from the chemical weathering of granite and basalt
The chemical weathering of silicate rocks can yield bicarbonate which is transported via
rivers to the ocean, followed by the deposition of carbonate, acting as a carbon sink on long …
rivers to the ocean, followed by the deposition of carbonate, acting as a carbon sink on long …
Climate controls on river chemistry
How does climate control river chemistry? Existing literature has examined extensively the
response of river chemistry to short‐term weather conditions from event to seasonal scales …
response of river chemistry to short‐term weather conditions from event to seasonal scales …
Influence of temporally varying weatherability on CO2-climate coupling and ecosystem change in the late Paleozoic
Earth's penultimate icehouse period, the late Paleozoic ice age (LPIA), was a time of
dynamic glaciation and repeated ecosystem perturbation, which was under conditions of …
dynamic glaciation and repeated ecosystem perturbation, which was under conditions of …
Snowmelt controls on concentration‐discharge relationships and the balance of oxidative and acid‐base weathering fluxes in an alpine catchment, E ast R iver, C …
Although important for riverine solute and nutrient fluxes, the connections between
biogeochemical processes and subsurface hydrology remain poorly characterized. We …
biogeochemical processes and subsurface hydrology remain poorly characterized. We …
Stable Isotopes and Bayesian Tracer Mixing Model Reveal Chemical Weathering and CO2 Release in the Jiulongjiang River Basin, Southeast China
Links between erosion, chemical weathering, and atmospheric CO2 can modulate the
global climate over geologic times, but the role of chemical weathering on Earth's long‐term …
global climate over geologic times, but the role of chemical weathering on Earth's long‐term …
Sulfate sulfur isotopes and major ion chemistry reveal that pyrite oxidation counteracts CO2 drawdown from silicate weathering in the Langtang-Trisuli-Narayani River …
Drawdown of atmospheric carbon dioxide (CO 2) due to silicate weathering in the Himalaya
has previously been implicated in Cenozoic cooling. However, over timescales shorter than …
has previously been implicated in Cenozoic cooling. However, over timescales shorter than …