South Atlantic deep-sea temperature evolution across the Pliocene-Pleistocene transition from clumped isotope thermometry

Autor: Elena Domínguez Valdés, Ilja Kocken, Tobias Agterhuis, Inigo Müller, Noa Bode, Dirk Kroon, Lucas Lourens, Martin Ziegler

The reconstruction of deep-ocean temperatures is key in the study of the different climate states in the geological past. Reconstructions covering the Pliocene-Pleistocene transition shed light on the global climatic change that followed the mid-Plio

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5ad46422bc0058dac62ab81341cb8c9d
https://doi.org/10.5194/egusphere-egu22-11222

Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years

Autor: Frank Peeters, Dirk Kroon, Gerald Ganssen, Pallavi Anand, Simon Jung, G-J A. Brummer, Brett Metcalfe

Publikováno v: Climate of the Past
Climate of the Past, 7(4), 1337-1349. European Geosciences Union
Ganssen, G M, Peeters, F J C, Metcalfe, B, Anand, P, Jung, S, Kroon, D & Brummer, G-J A 2011, ' Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years ', Climate of the Past, vol. 7, no. 4, pp. 1337-1349 . https://doi.org/10.5194/cp-7-1337-2011
Ganssen, G M, Peeters, F J C, Metcalfe, B, Anand, P, Jung, S J A, Kroon, D & Brummer, G J A 2011, ' Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years ', Climate of the Past, vol. 7, no. 4, pp. 1337-1349 . https://doi.org/10.5194/cpd-6-2795-2010, https://doi.org/10.5194/cp-7-1337-2011
Climate of the Past, Vol 7, Iss 4, Pp 1337-1349 (2011)

The oxygen isotopic composition of planktonic foraminifera tests is one of the widest used geochemical tools to reconstruct past changes of physical parameters of the upper ocean. It is common practice to analyze multiple individuals from a mono-spec

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::91493adf4647d8bdf33f24a11c916eda

Sea surface temperatures during the SW and NE monsoon seasons in the western Arabian Sea over the past 20,000 years

Autor: Margot Saher, Dirk Kroon, Frank Peeters

Publikováno v: Palaeogeography, Palaeoclimatology, Palaeoecology, 249(1-2), 216-228. Elsevier
Saher, M H, Peeters, F J C & Kroon, D 2007, ' Sea surface temperatures during the SW and NE monsoon seasons in the western Arabian Sea over the past 20,000 years. ', Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 249, no. 1-2, pp. 216-228 . https://doi.org/10.1016/j.palaeo.2007.01.014

The western Arabian Sea is influenced by the seasonal southwest and northeast monsoon wind systems. In the modern day, SW monsoon induced upwelling of cold water leads to lowest SSTs in summer, while in glacial periods, weakened upwelling and increas

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5efb70663495e2a50bcd0cbe2d67f62f
https://doi.org/10.1016/j.palaeo.2007.01.014

Stepwise Holocene aridification in NE Africa deduced from dust-borne radiogenic isotope records

Autor: Gerald Ganssen, Simon Jung, Dirk Kroon, Gareth Davies

Publikováno v: Earth and Planetary Science Letters, 221, 27-37. Elsevier
Jung, S J A, Davies, G R, Ganssen, G M & Kroon, D 2004, ' Stepwise Holocene aridification in NE Africa deduced from dust-borne radiogenic isotope records ', Earth and Planetary Science Letters, vol. 221, pp. 27-37 . https://doi.org/10.1016/S0012-821X(04)00095-0

Transfer of tropical heat to higher latitudes is the major driving force of the Earth's climate. Consequently, sediments in regions to the north and south of the tropics potentially retain an archive of past major climate reconfigurations. The climat

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::686254ddcaf7019f219f11e2bfe0e13a
https://doi.org/10.1016/s0012-821x(04)00095-0

Deep sea ventilation of the northeastern Atlantic during the last 15,000 years

Autor: William E. N. Austin, Dirk Kroon

Publikováno v: Global and Planetary Change, 30, 13-31. Elsevier
Austin, W E N & Kroon, D 2001, ' Deep sea ventilation of the northeastern Atlantic during the last 15,000 years. ', Global and Planetary Change, vol. 30, pp. 13-31 . https://doi.org/10.1016/S0921-8181(01)00074-1

Sea surface temperature and salinity estimates reconstructed from a core (56/-10/36) collected on the Barra Fan, northwest Scotland (56°43′N, 09°19′W; water depth 1320 m) show a series of rapid oscillations during the last deglacial period that

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ebdf3fdeeace57f908b820b6af71055a
https://research.vu.nl/en/publications/6eeb27c6-294b-40a4-9daa-e5850b035332