The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site

Ähnliche Einträge

• Response to “Comment on ‘The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site’"
  von: Lang, David C., et al.
  Veröffentlicht: (2014)
• Millennial‐scale climate variability in the subpolar North Atlantic Ocean during the late Pliocene
  Veröffentlicht: (2010)
• Limited exchange between the deep Pacific and Atlantic oceans during the warm mid-Pliocene and Marine Isotope Stage M2 “glaciation”
  von: Braaten, Anna Hauge, et al.
  Veröffentlicht: (2023)
• Deep-ocean circulation in the North Atlantic during the Plio-Pleistocene intensification of Northern Hemisphere Glaciation (~2.65-2.4 Ma)
  von: Jakob, Kim, et al.
  Veröffentlicht: (2021)
• North Atlantic midlatitude surface-circulation changes through the Plio-Pleistocene intensification of Northern Hemisphere glaciation
  von: Bolton, Clara T., et al.
  Veröffentlicht: (2018)