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Basalt weathering laws and the impact of basalt weathering on the global carbon cycle

TLDR
In this paper, the chemical weathering of basalts and the flux of carbon transferred from the atmosphere to the ocean during this major process at the surface of the Earth were investigated.
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This article is published in Chemical Geology.The article was published on 2003-12-30. It has received 762 citations till now. The article focuses on the topics: Soil production function & Weathering.

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The weathering and element fluxes from active volcanoes to the oceans: a Montserrat case study

TL;DR: The authors examined the impact of recent volcanic eruptions on the geochemistry of pre-existing hydrological systems and demonstrated that the initial chemical weathering yield of fresh volcanic material is higher than that from older deposits within the Lesser Antilles arc.
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Chemical weathering under mid- to cool temperate and monsoon-controlled climate: A study on water geochemistry of the Songhuajiang River system, northeast China

TL;DR: In this article, the authors studied the chemical weathering and CO2 consumption of the Songhuajiang Basin in a mid- to cool temperate and monsoon-controlled climatic zone.
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The influence of hydrothermal activity on the Li isotopic signature of rivers draining volcanic areas

TL;DR: In this article, the geochemistry and the isotopic composition of lithium (δ 7 Li) of rivers draining volcanic islands (Guadeloupe, Iceland, Java, Martinique and Sao Miguel) with a specific focus on continental hydrothermal activity were explored.
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River geochemistry, chemical weathering, and atmospheric CO2 consumption rates in the Virunga Volcanic Province (East Africa)

TL;DR: Water chemistry data from 13 rivers of the Virunga Volcanic Province (VVP) (Democratic Republic of Congo), sampled between December 2010 and February 2013, was reported in this article.
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Tectonic control of continental weathering, atmospheric CO2, and climate over Phanerozoic times

TL;DR: In this paper, the role of continental drift on the Phanerozoic evolution of the carbon cycle and climate with the GEOCLIM numerical model was explored, and it was shown that continental drift is a first order control parameter of the geological carbon cycle.
References
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Global silicate weathering and CO2 consumption rates deduced from the chemistry of large rivers

TL;DR: In this article, newly compiled data on the 60 largest rivers of the world are used to calculate the contribution of main lithologies, rain and atmosphere to river dissolved loads, and the relationship between the chemical weathering rates of silicates and the possible controlling parameters are explored.
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The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years

TL;DR: In this article, a computer model has been constructed that considers the effects on the CO/sub 2/ level of the atmosphere, and the Ca, Mg, and HCO/sub 3/ levels of the ocean, of the following processes: weathering on the continents of calcite, dolomite, and calcium-and-magnesium-containing silicates; biogenic precipitation and removal of CaCO 3/from the ocean; removal of Mg from the ocean via volcanic-seawater reaction; and the metamorphic-magmatic decarbon
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Tectonic forcing of late Cenozoic climate

TL;DR: In particular, tectonically driven increases in chemical weathering may have resulted in a decrease of atmospheric C02 concentration over the past 40 Myr as discussed by the authors. But this was not shown to be the case for the uplift of the Tibetan plateau and positive feedbacks initiated by this event.
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Geocarb III: A Revised Model of Atmospheric CO2 over Phanerozoic Time

TL;DR: In this article, the GEOCARB model has been updated with an emphasis on factors affecting CO2 uptake by continental weathering, including the role of plants in chemical weathering and the application of GCMs to study the long-term carbon cycle.
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A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature

TL;DR: In this article, it is suggested that the partial pressure of carbon dioxide in the atmosphere is buffered, over geological time scales, by a negative feedback mechanism, in which the rate of weathering of silicate minerals (followed by deposition of carbonate minerals) depends on surface temperature, which in turn depends on the carbon dioxide partial pressure through the greenhouse effect.
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