Browsing by Author "Jaeger, J.M."

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    • Integrated ocean drilling program expedition 341 Preliminary report: Southern Alaska margin- Interactions of tectonics, climate, and sedimentation 

      Jaeger, J.M.; Asahi, H.; Gulick, S.S.; Bahlburg, H.; LeVay, L.J.; Belanger, C.L.; Slagle, A.L.; Berbel, G.B.B.; Drab, L.; Childress, L.B.; Cowan, E.A.; Konno, S.; Forwick, M.; Marz, C.E.; Fukumura, A.; Matsuzaki, K.M.; Ge, S.; McClymont, E.L.; Gupta, S.M.; et al. (Integrated Ocean Drilling Program, 2013)
      Global climate during the Neogene is distinguished by the transition into a colder, more variable world dominated by the onset and intensification of major Northern Hemisphere glaciations. This transition to the icehouse ...

    • Mid-Pleistocene climate transition drives net mass loss from rapidly uplifting St. Elias mountains, Alaska 

      Gulick, S.P.S.; Jaeger, J.M.; Mix, A.C.; Asahi, H.; Bahlburg, H.; Belanger, C.L.; Berbel, G.B.B.; Childress, L.; Cowan, E.; Drab, L.; Forwick, M.; Fukumura, A.; Ge, S.; Gupta, S.M.; Kioka, A.; Konno, S.; LeVay, L.J.; Marz, C.; Matsuzaki, K.M.; McClymont, E.L.; Moy, C.; Muller, J.; Nakamura, A.; Ojima, T.; Ribeiro, F.R.; Ridgway, K.D.; Romero, O.E.; Slagle, A.L.; Stoner, J.S.; St-Onge, G.; Suto, I.; Walczak, M.D.; Worthington, L.L.; Bailey, I.; Enkelmann, E.; Reece, R.; Swartz, J.M. (National Academy of Sciences of the United States of America, 2015)
      Erosion, sediment production, and routing on a tectonically active continental margin reflect both tectonic and climatic processes; partitioning the relative importance of these processes remains controversial. Gulf of ...

    • Proceedings of the Integrated Ocean Drilling Program Vol. 341: Expedition reports Southern Alaska margin 

      Jaeger, J.M.; Gulick, S.P.S.; LeVay, L.J.; Asahi, H.; Bahlburg, H.; Belanger, C.L.; Berbel, G.B.B.; Childress, L.B.; Cowan, E.A.; Drab, L.; Forwick, M.; Fukumura, A.; Ge, S.; Gupta, S.M.; et. al. (Integrated Ocean Drilling Program, 2014)
      A remarkable expedition discovery is the substantial sediment volume accumulating on the shelf, slope, and deep sea fan since the early Pleistocene intensification of Northern Hemisphere glaciation and more significantly ...