Salt wedges and trapped brines of low-latitude endoreic saline lakes as potential modulators of GHG emission

Autor: Elisabeth Gibert-Brunet, Alina Tudryn, Ting Kong, Piotr Tucholka, Seyed-Hani Motavalli-Anbaran, Christelle Marlin, Aurélie Noret, Mohammad Lankarani, Hesam Ahmady-Birgani, Gilda Karimi

Publikováno v: Scientific Reports, Vol 13, Iss 1, Pp 1-12 (2023)

Abstract Large salt lakes are long-term witnesses to climatic conditions and land use in their basins. The majority are experiencing a drastic drop in water levels due to climate change and human impact. Endoreic Lake Urmia (NW Iran), the sixth large

Externí odkaz: https://doaj.org/article/6d72017afd4643b28f63e565fb77b011

Chronology of the Late Pleistocene Caspian Sea hydrologic changes: A review of dates and proposed climate-induced driving mechanisms

Autor: Alina Tudryn, Elisabeth Gibert-Brunet, Piotr Tucholka, Mikhail P. Antipov, Suzanne A.G. Leroy

Publikováno v: Quaternary Science Reviews
Quaternary Science Reviews, 2022, 293, pp.107672. ⟨10.1016/j.quascirev.2022.107672⟩
Quaternary Science Reviews, 2022, 293, ⟨10.1016/j.quascirev.2022.107672⟩

International audience; This paper provides a review of the dates used to define major hydrologic changes in the Caspian Sea during the Late Pleistocene that includes the Early Khvalynian and Hyrcanian highstands and the Atelian lowstand, and it disc

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3a6bdd93ada0524df6e0053f61ea9b57
https://cnrs.hal.science/hal-03874692/document

Formation and evolution of glauconite in the Demerara Contourite depositional system related to NADW circulation changes during late Quaternary (French Guiana)

Autor: Alina Tudryn, Pierre Giresse, Lies Loncke, Cédric Tallobre, Maria-Angela Bassetti, Germain Bayon, Roselyne Buscail, Sébastien Zaragosi

Publikováno v: Journal of South American Earth Sciences
Journal of South American Earth Sciences, Elsevier, 2019, 92, pp.167-183. ⟨10.1016/j.jsames.2019.03.011⟩
Journal Of South American Earth Sciences (0895-9811) (Elsevier BV), 2019-06, Vol. 92, P. 167-183

International audience; The Demerara Plateau is a marginal plateau which forms a bathymetric relief on the sea floor. Here, contourite deposits have been studied in detail, following the recent discovery of contourite sequences likely related to the

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::44ee500929f526297c5d971771e8e501
https://doi.org/10.1016/j.jsames.2019.03.011

Late Quaternary environmental changes of Lake Urmia basin (NW Iran) inferred from sedimentological and magnetic records

Autor: Mohammad Lankarani, Ting Kong, Elisabeth Gibert-Brunet, Alina Tudryn, Aurélie Noret, Marc Massault, Serge Miska, Piotr Tucholka, Hesam Ahmady-Birgani, Seyed-Hani Motavalli-Anbaran, Olivier Dufaure

Publikováno v: Quaternary International
Quaternary International, Elsevier, 2021, 589, pp.83-94. ⟨10.1016/j.quaint.2021.03.024⟩

International audience; The ongoing changes affecting Lake Urmia (NW Iran) are revealed by the lake water level decrease (~7 m in the last 20 yr) that was attributed to natural and anthropogenic causes but the exact impact of these factors on the sta

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76be3545d81c6e36fb6d00d70e0a92f3
https://hal.archives-ouvertes.fr/hal-03454996

Sedimentary archives of climate and sea-level changes during the Holocene in the Rhône prodelta (NW Mediterranean Sea)

Autor: Anne-Sophie Fanget, Maria-Angela Bassetti, Serge Berné, Alina Tudryn, Christophe Fontanier

Publikováno v: Climate of the Past, Vol 12, Iss 12, Pp 2161-2179 (2016)
Climate of the Past
Climate of the Past, European Geosciences Union (EGU), 2016, 12, pp.2161-2179. ⟨10.5194/cp-12-2161-2016⟩
Climate Of The Past (1814-9324) (Copernicus Gesellschaft Mbh), 2016-12, Vol. 12, N. 12, P. 2161-2179

A 7.38 m long sediment core was collected from the eastern section of the Rhône prodelta (NW Mediterranean) at 67 m water depth. A multi-proxy study (including sedimentary facies, benthic foraminifera, ostracods, and clay mineralogy) provides a mult

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::06ce73bcc42c13eb7df0340f7321f2a9
https://doi.org/10.5194/cp-12-2161-2016