Auflistung nach Mitwirkenden "Frank, Martin"
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Authigenic and Detrital Carbonate Nd Isotope Records Reflect Pulses of Detrital Material Input to the Labrador Sea During the Heinrich Stadials
Filippova, Alexandra; Frank, Martin; Kienast, Markus; Gutjahr, Marcus; Hathorne, Ed C.; Hillaire‐Marcel, Claude (Paleoceanography and Paleoclimatology, 2023-01-28)Limited constraints on the variability of the deep‐water production in the Labrador Sea complicate reconstructions of the strength of the Atlantic Meridional Overturning Circulation (AMOC) during the Late Quaternary. Large ... -
Enhanced Late Miocene Chemical Weathering and Altered Precipitation Patterns in the Watersheds of the Bay of Bengal Recorded by Detrital Clay Radiogenic Isotopes
Bretschneider, Lisa; Hathorne, Ed C.; Bolton, Clara T.; Gebregiorgis, Daniel; Giosan, Liviu; Gray, Emmeline; Huang, Huang; Holbourn, Ann; Kuhnt, Wolfgang; Frank, Martin (Paleoceanography and Paleoclimatology, 2021-09-06)The late Miocene was a period of declining CO2 levels and extensive environmental changes, which likely had a large impact on monsoon strength as well as on the weathering and erosion intensity in the South Asian Monsoon ... -
Persistent Provenance of South Asian Monsoon‐Induced Silicate Weathering Over the Past 27 Million Years
The development of the South Asian monsoon (SAM) and Himalaya‐Tibetan Plateau uplift were closely intertwined with some studies suggesting that uplift initiated the monsoon whereas others link tectonics with monsoon‐controlled ... -
Provenance and Weathering of Clays Delivered to the Bay of Bengal During the Middle Miocene: Linkages to Tectonics and Monsoonal Climate
Bretschneider, Lisa; Hathorne, Ed C.; Huang, Huang; Lübbers, Julia; Kochhann, Karlos G. D.; Holbourn, Ann; Kuhnt, Wolfgang; Thiede, Rasmus; Gebregiorgis, Daniel; Giosan, Liviu; Frank, Martin (Paleoceanography and Paleoclimatology, 2021-02-24)Tectonics and regional monsoon strength control weathering and erosion regimes of the watersheds feeding into the Bay of Bengal, which are important contributors to global climate evolution via carbon cycle feedbacks. The ...