Role of Southern Ocean sea ice on deep ocean circulation and carbon cycle at the Last Glacial Maximum

Fanny Lhardy

Open source

DOI: 10.70675/fb87b693z07e2z4ac4z9fbfz0c8b3e4ae719
Published: Not recorded
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Publisher: Agence Bibliographique de l'Enseignement Supérieur
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Cite this work

BibTeX

@article{allodium:10.70675/fb87b693z07e2z4ac4z9fbfz0c8b3e4ae719,
  title = {Role of Southern Ocean sea ice on deep ocean circulation and carbon cycle at the Last Glacial Maximum},
  author = {Fanny Lhardy},
  doi = {10.70675/fb87b693z07e2z4ac4z9fbfz0c8b3e4ae719},
  url = {https://doi.org/10.70675/fb87b693z07e2z4ac4z9fbfz0c8b3e4ae719}
}

RIS

TY  - JOUR
TI  - Role of Southern Ocean sea ice on deep ocean circulation and carbon cycle at the Last Glacial Maximum
AU  - Fanny Lhardy
DO  - 10.70675/fb87b693z07e2z4ac4z9fbfz0c8b3e4ae719
UR  - https://doi.org/10.70675/fb87b693z07e2z4ac4z9fbfz0c8b3e4ae719
ER  -

APA

Lhardy, F. (n.d.). Role of Southern Ocean sea ice on deep ocean circulation and carbon cycle at the Last Glacial Maximum. https://doi.org/10.70675/fb87b693z07e2z4ac4z9fbfz0c8b3e4ae719

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crossref · retrieved 2026-11-10T14:18:05.325Z