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Van Simaeys, Stefaan, Man, Ellen De, Vandenberghe, Noël, Brinkhuis, Henk, Steurbaut, Etienne (2004) Stratigraphic and palaeoenvironmental analysis of the Rupelian–Chattian transition in the type region: evidence from dinoflagellate cysts, foraminifera and calcareous nannofossils. Palaeogeography, Palaeoclimatology, Palaeoecology, 208 (1) 31-58 doi:10.1016/j.palaeo.2004.02.029

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Reference TypeJournal (article/letter/editorial)
TitleStratigraphic and palaeoenvironmental analysis of the Rupelian–Chattian transition in the type region: evidence from dinoflagellate cysts, foraminifera and calcareous nannofossils
JournalPalaeogeography, Palaeoclimatology, Palaeoecology
AuthorsVan Simaeys, StefaanAuthor
Man, Ellen DeAuthor
Vandenberghe, NoëlAuthor
Brinkhuis, HenkAuthor
Steurbaut, EtienneAuthor
Year2004 (May)Volume208
Issue1
PublisherElsevier BV
DOIdoi:10.1016/j.palaeo.2004.02.029Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID923708Long-form Identifiermindat:1:5:923708:1
GUID0
Full ReferenceVan Simaeys, Stefaan, Man, Ellen De, Vandenberghe, Noël, Brinkhuis, Henk, Steurbaut, Etienne (2004) Stratigraphic and palaeoenvironmental analysis of the Rupelian–Chattian transition in the type region: evidence from dinoflagellate cysts, foraminifera and calcareous nannofossils. Palaeogeography, Palaeoclimatology, Palaeoecology, 208 (1) 31-58 doi:10.1016/j.palaeo.2004.02.029
Plain TextVan Simaeys, Stefaan, Man, Ellen De, Vandenberghe, Noël, Brinkhuis, Henk, Steurbaut, Etienne (2004) Stratigraphic and palaeoenvironmental analysis of the Rupelian–Chattian transition in the type region: evidence from dinoflagellate cysts, foraminifera and calcareous nannofossils. Palaeogeography, Palaeoclimatology, Palaeoecology, 208 (1) 31-58 doi:10.1016/j.palaeo.2004.02.029
In(2004, May) Palaeogeography, Palaeoclimatology, Palaeoecology Vol. 208 (1) Elsevier BV

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Man, Ellen De, Simaeys, Stefaan Van, Vandenberghe, Noël, Harris, W. Burleigh, Wampler, J. Marion (2010) On the nature and chronostratigraphic position of the Rupelian and Chattian stratotypes in the southern North Sea basin. Episodes, 33 (1) 3-14 doi:10.18814/epiiugs/2010/v33i1/002
Abels, Hemmo A., Simaeys, Stefaan Van, Hilgen, Frits J., Man, Ellen De, Vandenberghe, Noël (2007) Obliquity-dominated glacio-eustatic sea level change in the early Oligocene: evidence from the shallow marine siliciclastic Rupelian stratotype (Boom Formation, Belgium). Terra Nova, 19 (1). 65-73 doi:10.1111/j.1365-3121.2006.00716.x
Brinkhuis, Henk (1994) Late Eocene to Early Oligocene dinoflagellate cysts from the Priabonian type-area (Northeast Italy): biostratigraphy and paleoenvironmental interpretation. Palaeogeography, Palaeoclimatology, Palaeoecology, 107 (1) 121-163 doi:10.1016/0031-0182(94)90168-6
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Van Simaeys, Stefaan, Munsterman, Dirk, Brinkhuis, Henk (2005) Oligocene dinoflagellate cyst biostratigraphy of the southern North Sea Basin. Review of Palaeobotany and Palynology, 134 (1). 105-128 doi:10.1016/j.revpalbo.2004.12.003
Friedrich, Oliver, Meier, K.J. Sebastian (2006) Suitability of stable oxygen and carbon isotopes of calcareous dinoflagellate cysts for paleoclimatic studies: Evidence from the Campanian/Maastrichtian cooling phase. Palaeogeography, Palaeoclimatology, Palaeoecology, 239 (3) 456-469 doi:10.1016/j.palaeo.2006.02.005
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Boonstra, M., Ramos, M.I.F., Lammertsma, E.I., Antoine, P.-O., Hoorn, C. (2015) Marine connections of Amazonia: Evidence from foraminifera and dinoflagellate cysts (early to middle Miocene, Colombia/Peru) Palaeogeography, Palaeoclimatology, Palaeoecology, 417. 176-194 doi:10.1016/j.palaeo.2014.10.032
Iakovleva, Alina I, Brinkhuis, Henk, Cavagnetto, Carla (2001) Late Palaeocene–Early Eocene dinoflagellate cysts from the Turgay Strait, Kazakhstan; correlations across ancient seaways. Palaeogeography, Palaeoclimatology, Palaeoecology, 172 (3) 243-268 doi:10.1016/s0031-0182(01)00300-5
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Ekdale, A.A. (2007) The application of ichnology to palaeoenvironmental and stratigraphic analysis. Palaeogeography, Palaeoclimatology, Palaeoecology, 251 (2) 321-322 doi:10.1016/j.palaeo.2007.03.003
 
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