Fate of Carbonates in the Earth’s Mantle (10-136 GPa)

Autor: Jing Gao, Xiang Wu, Xueyin Yuan, Wen Su

Publikováno v: Frontiers in Earth Science, Vol 10 (2022)

Earth carbon cycle shapes the evolution of our planet and our habitats. As a key region of carbon cycle, subduction zone acts as a sole channel transporting supracrustal carbonate rocks down to the mantle, balancing carbon budget between the Earth’

Externí odkaz: https://doaj.org/article/e210a1c965a841ffa36b43f1a15c7793

Acid digestion on river influenced shelf sediment organic matter: Carbon and nitrogen contents and isotopic ratios

Autor: Pierre Sansjofre, Oanez Lebeau, Marina Rabineau, Céline Liorzou, Virgil Pasquier

Publikováno v: Rapid Communications in Mass Spectrometry
Rapid Communications in Mass Spectrometry, Wiley, 2018, 32 (2), pp.86-92
Rapid Communications In Mass Spectrometry (0951-4198) (Wiley), 2018-01, Vol. 32, N. 2, P. 86-92
Rapid Communications in Mass Spectrometry, Wiley, 2018, 32 (2), pp.86-92. ⟨10.1002/rcm.8014⟩
Rapid Communications in Mass Spectrometry, 2018, 32 (2), pp.86-92. ⟨10.1002/rcm.8014⟩

Rationale Natural stable isotopes ratios (d13Corg and 15N vales) and associated elemental concentrations (i.e. total organic carbon and total nitrogen contents) preserved in marine sediments are frequently used for the determination of paleoenviro

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b4d2b66a8d802e38edf2b5da91e398d4
https://hal.univ-brest.fr/hal-01970149

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La fouille des enclos circulaires de l'âge du Bronze : une nouvelle approche ? Contribution géopédologique à l'étude des monuments arasés sur substrat limo-neux de Lauwin-Planque

Autor: Hélène Duvivier, Clara Samuelian, Olivier Collette, Emmanuelle Leroy-Langelin

Publikováno v: Bulletin de la Société Préhistorique Française
Bulletin de la Société Préhistorique Française, Société Préhistorique Française, 2011, 108 (1), pp.127-138
Bulletin de la Société préhistorique française
Bulletin de la Société préhistorique française, 2011, 108 (1), pp.127-138. ⟨10.3406/bspf.2011.13996⟩

The layer of carbonated silt (loess) found in Northern France is the result of wind sedimentation which developed during the periglacial climate of the Pleistocene. The decarbonatation of loess, active since 16,000 BP, is mainly climate-related. This

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4f59d8517a27a2c83b2e6325d3867a75
https://hal.archives-ouvertes.fr/hal-02873884

CO2 disposal into carbonate-dominated reservoirs: where and when Decarbonatation does occur ?

Autor: Garcia, Daniel, Moutte, Jacques, Michel, A., Trenty, L.

Publikováno v: MAMERN09: 3rd Int. Conf. on Approximation Methods and Numerical Modelling in Environment and Natural Resources
MAMERN09: 3rd Int. Conf. on Approximation Methods and Numerical Modelling in Environment and Natural Resources, Apr 2009, Pau, France. pp.473-476

International audience

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::85c507d88b541e90f52ddc557df32f13
https://shs.hal.science/halshs-01306826