Preservation of Fe/Mn‐redox fronts in sediments of an oligotrophic, oxygenated deep‐water lake (Lago Fagnano, Tierra del Fuego)-Reference-Cited by-同舟云学术

Preservation of Fe/Mn‐redox fronts in sediments of an oligotrophic, oxygenated deep‐water lake (Lago Fagnano, Tierra del Fuego)

Published:2022-02-24 Issue:4 Volume:69 Page:1841-1860
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Neugebauer Ina¹²^ORCID,Thomas Camille¹^ORCID,Ordoñez Luis¹^ORCID,Waldmann Nicolas D.³^ORCID,Recasens Cristina¹,Vizcaino Alexis⁴^ORCID,Jimenez‐Espejo Francisco J.⁵⁶^ORCID,Ariztegui Daniel¹^ORCID

Affiliation:

1. Department of Earth Sciences University of Geneva Rue des Maraichers 13 1205 Geneva Switzerland

2. Section Climate Dynamics and Landscape Evolution GFZ German Research Centre for Geosciences Telegrafenberg 14473 Potsdam Germany

3. Dr Moses Strauss Department of Marine Geosciences Charney School of Marine Sciences University of Haifa Mount Carmel 3498838 Haifa Israel

4. Department of Environmental Earth System Science Stanford University 67 Panama St Stanford CA 94305 USA

5. Instituto Andaluz de Ciencias de la Terra UGR‐CSIC Avda. de las Palmeras 4 18100 Armilla (Granada) Spain

6. Biogeochemistry Center Japan Agency for Marine‐Earth Science and Technology Natsushima‐cho 2‐15 Yokosuka 237‐0061 Japan

Funder

H2020 Marie Skłodowska-Curie Actions

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12976

Reference73 articles.

1. Radiocarbon Geochemistry of Modern and Ancient Arctic Lake Systems, Baffin Island, Canada

2. Carbon Cycling and Organic Radiocarbon Reservoir Effect in a Meromictic Crater Lake (Lac Pavin, Puy-de-Dôme, France)

3. Dominant ENSO frequencies during the Little Ice Age in Northern Patagonia: The varved record of proglacial Lago Frías, Argentina

4. Sedimentary pyrite formation

5. Sedimentary pyrite formation: An update

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