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Latest Cretaceous climatic and environmental change in the South Atlantic region: LATEST CRETACEOUS CHANGE SOUTH ATLANTIC
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“The obvious confluence of rapid volcanism preceding the KPgB, the severe δ 13 C perturbations in both oceanic and continental contemporary sediments and the LMWE cannot be coincidental.”
From Spatio-temporal volume recalibration shows Deccan volcanism caused Terminal Cretaceous Mass Extinction (2026) · cites this paper as Woelders et al., 2017
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Revised Carbonate-water isotopic temperature scale
EPSTEIN, S., BUCHSBAUM, R., LOWENSTAM, H. A., & UREY, H. C. (1953) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1953)64[1315:rcits]2.0.co;2 · Cited by 2,271
Petersen, S. V., Dutton, A., & Lohmann, K. C. (2016) · Nature Communications · doi:10.1038/ncomms12079 · Cited by 210
Triggering of the largest Deccan eruptions by the Chicxulub impact
Richards, M. A., Alvarez, W., Self, S., Karlstrom, L., Renne, P. R., Manga, M., Sprain, C. J., Smit, J., Vanderkluysen, L., & Gibson, S. A. (2015) · Geological Society of America Bulletin · doi:10.1130/b31167.1 · Cited by 210
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Research works printed but not linked: 105
- Abramovich, 2010, Global climate change and planktic foraminiferal response in the Maastrichtian, Paleoceanography, 25, 10.1029/2009PA001843 · DOI
- Açıkalın, 2015, Geochemical and palaeontological characterization of a new K-Pg boundary locality from the northern branch of the Neo-Tethys: Mudurnu-Göynük Basin, NW Turkey, Cretac. Res., 52, 251, 10.1016/j.cretres.2014.07.011 · DOI
- Alegret, 2005, Cretaceous/Paleogene boundary bathyal paleo-environments in the central North Pacific (DSDP Site 465), the Northwestern Atlantic (ODP Site 1049), the Gulf of Mexico and the Tethys: The benthic foraminiferal record, Palaeogeogr. Palaeoclimatol. Palaeoecol., 224, 53, 10.1016/j.palaeo.2005.03.031 · DOI
- Alegret, 2007, Deep-sea environments across the Cretaceous/Paleogene boundary in the eastern South Atlantic Ocean (ODP Leg 208, Walvis Ridge), Mar. Micropaleontol., 64, 1, 10.1016/j.marmicro.2006.12.003 · DOI
- Alvarez, 1980, Extraterrestrial cause for the Cretaceous-Tertiary extinction, Science, 208, 1095, 10.1126/science.208.4448.1095 · DOI · Paper page
- Anthonissen, 2012, The Geologic Time Scale 2012, 1083, 10.1016/B978-0-444-59425-9.15003-6 · DOI
- Archibald, 2010, Cretaceous extinctions: Multiple causes, Science, 328, 973, 10.1126/science.328.5981.973-a · DOI · Paper page
- Arregui, 2011, Geología y Recursos Naturales de la Provincia de Neuquén: XVIII Congreso Geológico Argentino, 29
- Baldoni, 1992, Palynology of the lower Lefipán formation (Upper Cretaceous) of Barranca de Los Perros, Chubut Province, Argentina. Part I, cryptogam spores and gymnosperm pollen, Palynology, 16, 117, 10.1080/01916122.1992.9989410 · DOI
- Ballent, 2008, Morphological abnormalities in late Cretaceous and early Paleocene foraminifer tests (northern Patagonia, Argentina), Mar. Micropaleontol., 67, 288, 10.1016/j.marmicro.2008.02.003 · DOI
- Barreda, 2007, Patagonian vegetation turnovers during the Paleogene-early Neogene: Origin of arid-adapted floras, Bot. Rev., 73, 31, 10.1663/0006-8101(2007)73[31:PVTDTP]2.0.CO;2 · DOI
- Barreda, 2012, Cretaceous/Paleogene floral turnover in Patagonia: Drop in diversity, low extinction, and a Classopollis spike, PLoS One, 7, 10.1371/journal.pone.0052455 · DOI
- Barrera, 1999, Evolution of the Cretaceous Ocean-Climate System, 332, 245, 10.1130/0-8137-2332-9.245 · DOI · Paper page
- Barrio, 1990, Paleogeographic control of upper cretaceous tidal deposits. Neuquén Basin, Argentina, J. South Am. Earth Sci., 3, 31, 10.1016/0895-9811(90)90016-T · DOI
- Bertels, 1964, Micropaleontología del Paleoceno de General Roca, provincia de Río Negro, Rev. del Mus. La Plata, Nueva Ser. Paleontol., 4, 125
- Bertels, 1975, Upper Cretaceous (Middle Maastrichtian) ostracodes of Argentina, Micropaleontology, 21, 97, 10.2307/1485157 · DOI
- Bertels, 1979, Paleobiogeografía de los Foraminíferos del Cretácico superior y Cenozoico de America del Sur, Ameghiniana, 16, 273
- Birch, 2016, Partial collapse of the marine carbon pump after the Cretaceous-Paleogene boundary, Geology, 44, 287, 10.1130/G37581.1 · DOI
- Boucot, 2013, Phanerozoic Paleoclimate: Concepts in Sedimentology and Paleontology, 11, 1
- Brezina, 2014, Boring polychaetes associated with Pycnodonte (Phygraea) vesicularis (lamarck) from the Upper Cretaceous of Patagonia. A case of commensalism?, Ameghiniana, 51, 129, 10.5710/AMGH.04.12.2013.1266 · DOI
- Brinkhuis, 1988, Dinoflagellate cysts, sea level changes and planktonic foraminifers across the Cretaceous-Tertiary boundary at El Haria, northwest Tunisia, Mar. Micropaleontol., 13, 153, 10.1016/0377-8398(88)90002-3 · DOI
- Brugger, 2016, Baby, it's cold outside: Climate model simulations of the effects of the asteroid impact at the end of the Cretaceous, Geophys. Res. Lett., 44, 419, 10.1002/2016GL072241 · DOI · Paper page
- Bush, 1997, The Late Cretaceous: Simulation with a coupled atmosphere-ocean GCM, Paleoceanography, 21, 475
- Buzas, 1993, A statistical evaluation of the microhabitats of living (stained) infaunal benthic foraminifera, Mar. Micropaleontol., 20, 311, 10.1016/0377-8398(93)90040-5 · DOI
- Chumakov, 1995, Climatic zones in the middle of the Cretaceous Period, Stratigr. Geol. Correl., 3, 3
- Compagnucci, 2011, Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios, Biol. J. Linn. Soc., 103, 229, 10.1111/j.1095-8312.2011.01655.x · DOI
- Corliss, 1985, Microhabitats of benthic foraminifera within deep-sea sediments, Nature, 314, 435, 10.1038/314435a0 · DOI
- Corliss, 1988, Morphotype patterns of Norwegian Sea deep-sea benthic foraminifera and ecological implications, Geology, 16, 716, 10.1130/0091-7613(1988)016<0716:MPONSD>2.3.CO;2 · DOI · Paper page
- Culver, 2003, Benthic foraminifera across the Cretaceous-Tertiary (K-T) boundary: A review, Mar. Micropaleontol., 47, 177, 10.1016/S0377-8398(02)00117-2 · DOI
- Cushman , J. A. 1946 Upper Cretaceous foraminifera of the Gulf Region of the United States and adjacent areas Geol. Surv. Prof. Pap. 206 · DOI
- Dinarès-Turell, 2013, Detailed correlation and astronomical forcing across the Upper Maastrichtian succession from the Basque Basin, Bol. Geol. y Min., 124, 253
- Dinarès-Turell, 2014, Astronomical calibration of the Danian stage (early Paleocene) revisited: Settling chronologies of sedimentary records across the Atlantic and Pacific Oceans, Earth Planet. Sci. Lett., 405, 119, 10.1016/j.epsl.2014.08.027 · DOI
- Fensome, 2008, DINOFLAJ2, version 1. American Association of Stratigraphic Palynologists, Data Series no., 1
- Folguera, 2011, Geología y Recursos Naturales De La Provincia de Neuquén: XVIII Congreso Geológico Argentino, 275
- Gibson, 1973, Species diversity: Patterns in modern and Miocene foraminifera of the eastern margin of North America, Geol. Soc. Am. Bull., 84, 217, 10.1130/0016-7606(1973)84<217:SDPIMA>2.0.CO;2 · DOI · Paper page
- De Gracianski, 1998, Mesozoic-Cenozoic Sequence Stratigraphy of European Basins, 60, 786, 10.2110/pec.98.60 · DOI
- Habib, 2007, The Manumiella seelandica global spike: Cooling during regression at the close of the Maastrichtian, Palaeogeogr. Palaeoclimatol. Palaeoecol., 255, 87, 10.1016/j.palaeo.2007.02.043 · DOI
- Hayek, 2013, On the proper and efficient use of diversity measures with individual field samples, J. Foraminifer. Res., 43, 305, 10.2113/gsjfr.43.3.305 · DOI
- Henehan, 2016, Biogeochemical significance of pelagic ecosystem function: An end-Cretaceous case study, Philos. Trans. R. Soc. B, 371, 10.1098/rstb.2015.0510 · DOI · Paper page
- Henriksson, 1993, Biochronology of the terminal Cretaceous calcareous nannofossil zone of Micula prinsii, Cretac. Res., 14, 59, 10.1006/cres.1993.1005 · DOI
- Hopmans, 2004, A novel proxy for terrestrial organic matter in sediments based on branched and isoprenoid tetraether lipids, Earth Planet. Sci. Lett., 224, 107, 10.1016/j.epsl.2004.05.012 · DOI
- Hopmans, 2016, The effect of improved chromatography on GDGT-based palaeoproxies, Org. Geochem., 93, 1, 10.1016/j.orggeochem.2015.12.006 · DOI
- Iglesias, 2007, A Paleocene lowland macroflora from Patagonia reveals significantly greater richness than North American analogs, Geology, 35, 947, 10.1130/G23889A.1 · DOI
- Johnson, 2016, A progressively wetter climate in southern East Africa over the past 1.3 million years, Nature, 537, 220, 10.1038/nature19065 · DOI
- Jorissen, 1995, A conceptual model explaining benthic foraminiferal microhabitats, Mar. Micropaleontol., 26, 3, 10.1016/0377-8398(95)00047-X · DOI
- Jorissen, 2007, Proxies in Late Cenozoic Paleoceanography: Pt. 2: Biological Tracers and Biomarkers, 263, 10.1016/S1572-5480(07)01012-3 · DOI
- Keller, 2007, High stress late Maastrichtian-Early Danian palaeoenvironment in the Neuquén Basin, Argentina, Cretac. Res., 28, 939, 10.1016/j.cretres.2007.01.006 · DOI
- Keller, 2016, Upheavals during the Late Maastrichtian: Volcanism, climate and faunal events preceding the end-Cretaceous mass extinction, Palaeogeogr. Palaeoclimatol. Palaeoecol., 441, 137, 10.1016/j.palaeo.2015.06.034 · DOI
- Kellough, 1965, Paleoecology of the foraminiferida of the Wills Point Formation (Midway Group) in Northeast Texas, Trans. Gulf Coast Assoc. Geol. Soc., 15, 73
- Kemp, 2014, A cool temperate climate on the Antarctic Peninsula through the latest Cretaceous to early Paleogene, Geology, 42, 583, 10.1130/G35512.1 · DOI · Paper page
- Kiessling, 2005, Massive corals in Paleocene siliciclastic sediments of Chubut (Argentina), Facies, 51, 233, 10.1007/s10347-005-0023-3 · DOI
- Kiessling, 2006, A Maastrichtian microbial reef and associated limestones in the Roca Formation of Patagonia (Neuquén Province, Argentina), Foss, Rec. - Mitteilungen aus dem Museum für Naturkd., 9, 183, 10.1002/mmng.200600007 · DOI
- Kim, 2010, New indices and calibrations derived from the distribution of crenarchaeal isoprenoid tetraether lipids: Implications for past sea surface temperature reconstructions, Geochim. Cosmochim. Acta, 74, 4639, 10.1016/j.gca.2010.05.027 · DOI
- Kring, 2007, The Chicxulub impact event and its environmental consequences at the Cretaceous-Tertiary boundary, Palaeogeogr. Palaeoclimatol. Palaeoecol., 255, 4, 10.1016/j.palaeo.2007.02.037 · DOI
- Kuiper, 2008, Synchronizing rock clocks of Earth history, Science, 320, 500, 10.1126/science.1154339 · DOI · Paper page
- Labraga, 1997, The climate change in South America due to a doubling in the CO2 concentration: Intercomparison of general circulation model equilibrium experiments, Int. J. Climatol., 17, 377, 10.1002/(SICI)1097-0088(19970330)17:4<377::AID-JOC129>3.0.CO;2-P · DOI
- Laskar, 2011, Strong chaos induced by close encounters with Ceres and Vesta, Astron. Astrophys., 532, L4, 10.1051/0004-6361/201117504 · DOI · Paper page
- Li, 1998, Abrupt deep-sea warming at the end of the Cretaceous, Geology, 26, 995, 10.1130/0091-7613(1998)026<0995:ADSWAT>2.3.CO;2 · DOI
- Machalski, 2016, Late Maastrichtian cephalopods, dinoflagellate cysts and foraminifera from the Cretaceous-Paleogene succession at Lechówka, southeast Poland: Stratigraphic and environmental implications, Cretac. Res., 57, 208, 10.1016/j.cretres.2015.08.012 · DOI
- Malumián, 2011, The Late Cretaceous-Cenozoic transgressions in Patagonia and the Fuegian Andes: Foraminifera, palaeoecology, and palaeogeography, Biol. J. Linn. Soc., 103, 269, 10.1111/j.1095-8312.2011.01649.x · DOI
- Ménot, 2006, Early reactivation of European rivers during the last deglaciation, Science, 313, 1623, 10.1126/science.1130511 · DOI
- Murray, 2006, Ecology and Applications of Benthic Foraminifera, 426, 10.1017/CBO9780511535529 · DOI
- Nordt, 2003, Terrestrial evidence for two greenhouse events in the latest Cretaceous, GSA Today, 13, 4, 10.1130/1052-5173(2003)013<4:TEFTGE>2.0.CO;2 · DOI
- Olsson, 2001, Paleobiogeography of Pseudotextularia elegans during the latest Maastrichtian global warming event, J. Foraminifer. Res., 31, 275, 10.2113/31.3.275 · DOI
- Olsson, 2002, Catastrophic Events and Mass Extinctions: Impacts and Beyond, 356, 97, 10.1130/0-8137-2356-6.97 · DOI
- Palazzesi, 2007, Major vegetation trends in the Tertiary of Patagonia (Argentina): A qualitative paleoclimatic approach based on palynological evidence, Flora-morphology, Distrib. Funct. Ecol. Plants, 202, 328, 10.1016/j.flora.2006.07.006 · DOI
- Papú, 1996, Simposio Paleogeno de América del Sur Buenos Aires. Actas Subsecretaria de Mineria de la Nación, Anales, 33, 17
- Prámparo, 2006, Late Maastrichtian dinoflagellate cysts from the Cerro Butaló section, southern Mendoza province, Argentina, J. Micropaleontol., 25, 23, 10.1144/jm.25.1.23 · DOI
- Prámparo, 2014, Sharks (Neoselachii) and palynomorphs from Mendoza (Argentina): New evidence of the Late Cretaceous Atlantic marine transgression, Alcheringa An Australas, J. Palaeontol., 38, 177, 10.1080/03115518.2014.849027 · DOI
- Punekar, 2016, A multi-proxy approach to decode the end-Cretaceous mass extinction, Palaeogeogr. Palaeoclimatol. Palaeoecol., 441, 116, 10.1016/j.palaeo.2015.08.025 · DOI
- Ravizza, 2003, Chemostratigraphic evidence of Deccan volcanism from the marine osmium isotope record, Science, 302, 1392, 10.1126/science.1089209 · DOI · Paper page
- Renne, 2013, Time scales of critical events around the Cretaceous-Paleogene boundary, Science, 339, 684, 10.1126/science.1230492 · DOI · Paper page
- Saint-Marc, 1988, A quantitative analysis of Paleocene benthic foraminiferal assemblages in central Tunisia, J. Foraminifer. Res., 18, 97, 10.2113/gsjfr.18.2.97 · DOI
- Scasso, 2005, A tsunami deposit at the Cretaceous/Paleogene boundary in the Neuquén Basin of Argentina, Cretac. Res., 26, 283, 10.1016/j.cretres.2004.12.003 · DOI
- Scasso, 2012, Integrated bio- and lithofacies analysis of coarse-grained, tide-dominated deltaic environments across the Cretaceous/Paleogene boundary in Patagonia, Argentina, Cretac. Res., 36, 37, 10.1016/j.cretres.2012.02.002 · DOI
- Schiøler, 1997, Dinoflagellate biostratigraphy and sequence stratigraphy of the type Maastrichtian (Upper Cretaceous), ENCI quarry, The Netherlands, Mar. Micropaleontol., 31, 65, 10.1016/S0377-8398(96)00058-8 · DOI
- Schmidt, 2016, Selective environmental stress from sulphur emitted by continental flood basalt eruptions, Nat. Geosci., 9, 77, 10.1038/ngeo2588 · DOI · Paper page
- Schoene, 2015, U-Pb geochronology of the Deccan Traps and relation to the end-Cretaceous mass extinction, Science, 347, 9, 10.1126/science.aaa0118 · DOI · Paper page
- Schouten, 2002, Distributional variations in marine crenarchaeotal membrane lipids: A new tool for reconstructing ancient sea water temperatures?, Earth Planet. Sci. Lett., 204, 265, 10.1016/S0012-821X(02)00979-2 · DOI
- Schouten, 2013, The organic geochemistry of glycerol dialkyl glycerol tetraether lipids: A review, Org. Geochem., 54, 19, 10.1016/j.orggeochem.2012.09.006 · DOI
- Schulte, 2006, The Cretaceous-Paleogene (K-P) boundary at Brazos, Texas: Sequence stratigraphy, depositional events and the Chicxulub impact, Sediment. Geol., 184, 77, 10.1016/j.sedgeo.2005.09.021 · DOI
- Schulte, 2010, The Chicxulub asteroid impact and mass extinction at the Cretaceous-Paleogene boundary, Science, 327, 1214, 10.1126/science.1177265 · DOI · Paper page
- Shackleton, 1975, Paleotemperature history of the Cenozoic and the initiation of Antarctic glaciation: Oxygen and carbon isotope analyses in DSDP Sites 277, 279, and 281, Initial Reports Deep Sea Drill. Proj., 29, 743
- Sluijs, 2009, A dynamic climate and ecosystem state during the Paleocene-Eocene Thermal Maximum: Inferences from dinoflagellate cyst assemblages on the New Jersey Shelf, Biogeosciences, 6, 1755, 10.5194/bg-6-1755-2009 · DOI
- Sluijs, 2005, From greenhouse to icehouse; organic-walled dinoflagellate cysts as paleoenvironmental indicators in the Paleogene, Earth-Science Rev., 68, 281, 10.1016/j.earscirev.2004.06.001 · DOI
- Speijer, 1996, Biotic Recovery From Mass Extinction Events, 343
- Thibault, 2010, The calcareous nannofossil response to the end-Cretaceous warm event in the tropical Pacific, Palaeogeogr. Palaeoclimatol. Palaeoecol., 291, 239, 10.1016/j.palaeo.2010.02.036 · DOI
- Thibault, 2016, Climatic fluctuations and sea-surface water circulation patterns at the end of the Cretaceous era: Calcareous nannofossil evidence, Palaeogeogr. Palaeoclimatol. Palaeoecol., 441-1, 152, 10.1016/j.palaeo.2015.07.049 · DOI
- Tobin, 2012, Extinction patterns, δ18O trends, and magnetostratigraphy from a southern high-latitude Cretaceous-Paleogene section: Links with Deccan volcanism, Palaeogeogr. Palaeoclimatol. Palaeoecol., 350-352, 180, 10.1016/j.palaeo.2012.06.029 · DOI · Paper page
- Torsvik, 2012, Phanerozoic polar wander, palaeogeography and dynamics, Earth-Science Rev., 114, 325, 10.1016/j.earscirev.2012.06.007 · DOI
- Tunik, 2010, Early uplift and orogenic deformation in the Neuquén Basin: Constraints on the Andean uplift from U-Pb and Hf isotopic data of detrital zircons, Tectonophysics, 489, 258, 10.1016/j.tecto.2010.04.017 · DOI
- Hinsbergen, 2015, A paleolatitude calculator for paleoclimate studies, PLoS One, 10, 10.1371/journal.pone.0126946 · DOI
- Vandenberghe, 2012, The Geologic Time Scale 2012, 855, 10.1016/B978-0-444-59425-9.00028-7 · DOI
- Vellekoop, 2014, Rapid short-term cooling following the Chicxulub impact at the Cretaceous-Paleogene boundary, Proc. Natl. Acad. Sci. U. S. A., 111, 7537, 10.1073/pnas.1319253111 · DOI · Paper page
- Vellekoop, 2015, Palynological evidence for prolonged cooling along the Tunisian continental shelf following the K-Pg boundary impact, Palaeogeogr. Palaeoclimatol. Palaeoecol., 426, 216, 10.1016/j.palaeo.2015.03.021 · DOI
- Vellekoop, 2016, Evidence for Cretaceous-Paleogene boundary bolide “impact winter” conditions from New Jersey, USA, Geology, 44, 619, 10.1130/G37961.1 · DOI
- Vera, 2006, Climate change scenarios for seasonal precipitation in South America from IPCC-AR4 models, Geophys. Res. Lett., 33, 10.1029/2006GL025759 · DOI
- Villalba, 1998, Tree-ring evidence for long-term precipitation changes in subtropical South America, Int. J. Climatol., 18, 1463, 10.1002/(SICI)1097-0088(19981115)18:13<1463::AID-JOC324>3.0.CO;2-A · DOI
- Weijers, 2006, Occurrence and distribution of tetraether membrane lipids in soils: Implications for the use of the TEX86 proxy and the BIT index, Org. Geochem., 37, 1680, 10.1016/j.orggeochem.2006.07.018 · DOI
- Westerhold, 2008, Astronomical calibration of the Paleocene time, Palaeogeogr. Palaeoclimatol. Palaeoecol., 257, 377, 10.1016/j.palaeo.2007.09.016 · DOI · Paper page
- Wilf, 2003, Correlated terrestrial and marine evidence for global climate changes before mass extinction at the Cretaceous-Paleogene boundary, Proc. Natl. Acad. Sci. U. S. A., 100, 599, 10.1073/pnas.0234701100 · DOI · Paper page
- Williams, 2004, Proceedings of the Ocean Drilling Program. Scientific Results, 189, 1
- Witts, 2016, Macrofossil evidence for a rapid and severe Cretaceous-Paleogene mass extinction in Antarctica, Nat. Commun., 7, 10.1038/ncomms11738 · DOI
- Woelders, 2015, Stable seafloor conditions, sea level and food supply during the latest Maastrichtian at Brazos River, Texas, Mar. Micropaleontol., 121, 41, 10.1016/j.marmicro.2015.10.002 · DOI
- Zachos, 2004, Proceedings of the Ocean Drilling Program, Initial Rep., 208, 10.2973/odp.proc.ir.208.2004 · DOI
Cited by
Kale, V. S., Upasani, D., Rajput, M., Dole, G., & Pillai, S. P. (2026) · Geological Society of America Bulletin · doi:10.1130/b38412.1 · Cited by 3
Metadata
- Authors
- Woelders, L., Vellekoop, J., Kroon, D., Smit, J., Casadío, S., Prámparo, M. B., Dinarès-Turell, J., Peterse, F., Sluijs, A., Lenaerts, J. T. M., & Speijer, R. P.
- Affiliations
- Department of Earth and Environmental Sciences; KU Leuven; Leuven Belgium
- School of GeoSciences, Grant Institute; University of Edinburgh; Edinburgh UK
- Event Stratigraphy; VU University Amsterdam; Amsterdam Netherlands
- CONICET, Universidad Nacional de Rio Negro; General Roca Argentina
- IANIGLA CCT-CONICET; Mendoza Argentina
- Istituto Nazionale di Geofisica e Vulcanologia; Rome Italy
- Department of Earth Sciences, Faculty of Geosciences; Utrecht University; Utrecht Netherlands
- Institute for Marine and Atmospheric Research; Utrecht University; Utrecht Netherlands
- ORCID
- Venue
- Paleoceanography
- Publisher
- American Geophysical Union (AGU)
- Published
- 2017-05
- Volume
- 32
- Issue
- 5
- Pages
- 466-483
- ISSN
- 0883-8305
- Cited by
- 74
- References
- 3
- Language
- en
- Licence
- Funders
- Fonds Wetenschappelijk Onderzoek (G.0B85.13)
- European Research Council (259627)
- Nederlandse Organisatie voor Wetenschappelijk Onderzoek (834.11.006)
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