Evidence for a Northern Hemispheric trigger of the 100,000-y glacial cyclicity

Autor: Alberto Malinverno, M. Yehudai, Leopoldo D. Pena, J. Kim, Steven L. Goldstein, Maria Jaume-Seguí, Louise Bolge, K. P. Knudson, Torsten Bickert

Publikováno v: Proc Natl Acad Sci U S A

The causes of the Mid-Pleistocene Transition, the shift from ∼41-ky to 100-ky interglacial–glacial cycles and more intense ice ages, remain intensely debated, as this fundamental change occurred between ∼1,250 and 650 ka without substantial cha

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d25143cc9c511ff99cd3bb0ff94c88ad
https://doi.org/10.1073/pnas.2020260118

The Atlantic Meridional Overturning Circulation Over Time From Nd Isotopes

Autor: Steve Goldstein, Leo D. Pena, Chandranath Basak, R. Lupien, J. Kim, K. P. Knudson, Maria Jaume-Seguí, Allison E. Hartman, M. Yehudai

The Atlantic Meridional Overturning Circulation (AMOC) brings heat from the tropics to the high latitudes, and its temporal variability has major impacts on climatic cycles. We have constructed north-south profiles using deep sea cores from the North

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6e4794bda3c1bb37d5150f65515693f9
https://doi.org/10.5194/egusphere-egu2020-13297

Last interglacial sea levels and regional tectonics from fossil coral reefs in the northeast Gulf of Aqaba

Autor: Mordechai Stein, M. Yehudai, N. Bar, Amotz Agnon, Boaz Lazar, Y. Shaked

Publikováno v: Quaternary Science Reviews. 191:41-56

Elevated reef terraces in the northeast Gulf of Aqaba (GOA) constrain the history of tectonic uplift and local relative sea level changes during the last interglacial period. These relative sea level changes were inferred from measured elevations cou

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::7013db9b404715168692d1c5cbf8c3d0
https://doi.org/10.1016/j.quascirev.2018.04.031

Deep Atlantic Ocean carbon storage and the rise of 100,000-year glacial cycles

Autor: Maria Jaume-Seguí, Jesse Farmer, L. Haynes, Bärbel Hönisch, Steven L. Goldstein, David B Bell, Maureen E. Raymo, J. Kim, Simon Jung, Leopoldo D. Pena, M. Yehudai, Dick Kroon, Heather L Ford

Publikováno v: Farmer, J R, Hönisch, B, Haynes, L L, Kroon, D, Jung, S, Ford, H L, Raymo, M E, Jaume-Segui, M, Bell, D, Goldstein, S L, Pena, L D, Yehudai, M & Kim, J 2019, ' Deep Atlantic Ocean carbon storage and the rise of 100,000-year glacial cycles ', Nature Geoscience, vol. 12, pp. 355-360 . https://doi.org/10.1038/s41561-019-0334-6

Over the past three million years, Earth’s climate oscillated between warmer interglacials with reduced terrestrial ice volume and cooler glacials with expanded polar ice sheets. These climate cycles, as reflected in benthic foraminiferal oxygen is

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::711ff323c16b2e535dc19b2fb5177420
https://www.pure.ed.ac.uk/ws/files/80717146/80717087._Kroon._AAM.pdf

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