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Lithium isotope geochemistry
The lithium isotope system is increasingly being applied to a variety of Earth science studies,
as the burgeoning literature attests; over 180 papers have been published in the last twelve …
as the burgeoning literature attests; over 180 papers have been published in the last twelve …
A Cenozoic record of deep oceanic Zn isotopic composition in ferromanganese crusts
Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …
[KNIHA][B] Stable isotope geochemistry
J Hoefs, J Hoefs - 2009 - Springer
The nine editions of Stable Isotope Geochemistry have appeared over a time span of nearly
50 years. The first edition (1973) appeared as a slim book of 135 pages. Due to the rapid …
50 years. The first edition (1973) appeared as a slim book of 135 pages. Due to the rapid …
Riverine Li isotope fractionation in the Amazon River basin controlled by the weathering regimes
We report Li isotope composition (δ 7 Li) of river-borne dissolved and solid material in the
largest River system on Earth, the Amazon River basin, to characterize Li isotope …
largest River system on Earth, the Amazon River basin, to characterize Li isotope …
Hydrological control of river and seawater lithium isotopes
Seawater lithium isotopes (δ7Li) record changes over Earth history, including a∼ 9‰
increase during the Cenozoic interpreted as reflecting either a change in continental silicate …
increase during the Cenozoic interpreted as reflecting either a change in continental silicate …
Experimental constraints on Li isotope fractionation during clay formation
Abstract Knowledge of the lithium (Li) isotope fractionation factor during clay mineral
formation is a key parameter for Earth system models. This study refines our understanding …
formation is a key parameter for Earth system models. This study refines our understanding …
Enhanced clay formation key in sustaining the Middle Eocene Climatic Optimum
Abstract The Middle Eocene Climatic Optimum (around 40 million years ago) was a roughly
400,000-year-long global warming phase associated with an increase in atmospheric CO2 …
400,000-year-long global warming phase associated with an increase in atmospheric CO2 …
Experimental investigation of lithium isotope fractionation during kaolinite adsorption: Implications for chemical weathering
The feedback between CO 2 sources and sinks through chemical weathering is one of the
important reasons why Earth has maintained a habitable climate for over four billion years …
important reasons why Earth has maintained a habitable climate for over four billion years …
Lithium-isotope evidence for enhanced silicate weathering during OAE 1a (Early Aptian Selli event)
An abrupt rise in temperature, forced by a massive input of CO 2 into the atmosphere, is
commonly invoked as the main trigger for Oceanic Anoxic Events (OAEs). Global warming …
commonly invoked as the main trigger for Oceanic Anoxic Events (OAEs). Global warming …
[KNIHA][B] Iron geochemistry: an isotopic perspective
Iron is a remarkable element in its relatively high abundance for its mass and its sensitivity to
(and control of) redox on a planetary scale over geologic time. Numerous volumes have …
(and control of) redox on a planetary scale over geologic time. Numerous volumes have …