Southern Hemisphere Westerly Winds have modulated the formation of laminations in sediments in Lago Fagnano (Tierra del Fuego, Argentina) over the past 6.3 ka-Reference-Cited by-同舟云学术

Southern Hemisphere Westerly Winds have modulated the formation of laminations in sediments in Lago Fagnano (Tierra del Fuego, Argentina) over the past 6.3 ka

Published:2022-09-18 Issue:1 Volume:52 Page:124-138
ISSN:0300-9483
Container-title:Boreas
language:en
Short-container-title:Boreas

Author:

Vizcaino Alexis¹^ORCID,Jimenez‐Espejo Francisco J.²³^ORCID,Dunbar Robert B.¹^ORCID,Mucciarone David¹^ORCID,García‐Alix Antonio⁴^ORCID,Neugebauer Ina⁵⁶^ORCID,Ariztegui Daniel⁵^ORCID

Affiliation:

1. Earth System Science Stanford University 397 Panama Mall Stanford CA 94305 California USA

2. Instituto Andaluz de Ciencias de la Tierra, UGR‐CSIC Avda. de las Palmeras, n° 4 Armilla 18100 Spain

3. Research Institute for Marine Resources Utilization (Biogeochemistry Program), Japan Agency for Marine‐Earth Science and Technology 2‐15 Natsushimacho Yokosuka Kanagawa 237‐0061 Japan

4. Department Paleontología y Estratigrafía Universidad de Granada Avenida de la Fuente Nueva S/N, 18071 Granada Spain

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

6. Section Climate Dynamics and Landscape Evolution, GFZ German Research Centre for Geosciences, Wissenschaftpark “Albert Einstein” Telegrafenberg 14473 Potsdam Germany

Funder

Ministerio de Ciencia e Innovación

Publisher

Wiley

Subject

Geology,Archeology,Ecology, Evolution, Behavior and Systematics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12600

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3. Deciphering bottom current velocity and paleoclimate signals from contourite deposits in the Gulf of Cádiz during the last 140 kyr: An inorganic geochemical approach

4. Postglacial fluctuations of Cordillera Darwin glaciers (southernmost Patagonia) reconstructed from Almirantazgo fjord sediments

5. Multiproxy record of Holocene paleoenvironmental change, Tierra del Fuego, Argentina

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