The Rupelian is, in the
geologic timescale
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochr ...
, the older of two
ages or the lower of two
stages
Stage or stages may refer to:
Acting
* Stage (theatre), a space for the performance of theatrical productions
* Theatre, a branch of the performing arts, often referred to as "the stage"
* ''The Stage'', a weekly British theatre newspaper
* S ...
of the
Oligocene Epoch
In chronology and periodization, an epoch or reference epoch is an instant in time chosen as the origin of a particular calendar era. The "epoch" serves as a reference point from which time is measured.
The moment of epoch is usually decided by ...
/
Series
Series may refer to:
People with the name
* Caroline Series (born 1951), English mathematician, daughter of George Series
* George Series (1920–1995), English physicist
Arts, entertainment, and media
Music
* Series, the ordered sets used in ...
. It spans the time between . It is preceded by the
Priabonian Stage (part of the Eocene) and is followed by the
Chattian Stage.
Name
The stage is named after the small river
Rupel
The Rupel () is a tidal river in northern Belgium, right tributary of the Scheldt. It is about long. It flows through the Belgian province of Antwerp. It is formed by the confluence of the rivers Dijle and Nete, in Rumst. It flows into the Sche ...
in Belgium, a tributary to the
Scheldt
The Scheldt (french: Escaut ; nl, Schelde ) is a river that flows through northern France, western Belgium, and the southwestern part of the Netherlands, with its mouth at the North Sea. Its name is derived from an adjective corresponding to ...
. The Belgian
Rupel Group
The Rupel Group is a stratigraphic group of rock strata in the subsurface of Belgium. It is subdivided into three formations that are all marine deposits (sands and clays) of Oligocene age.
Name
The Rupel Group was first named by Belgian geologis ...
derives its name from the same source. The name Rupelian was introduced in scientific literature by Belgian geologist
André Hubert Dumont
André — sometimes transliterated as Andre — is the French and Portuguese form of the name Andrew, and is now also used in the English-speaking world. It used in France, Quebec, Canada and other French-speaking countries. It is a variation ...
in 1850. The separation between the
group
A group is a number of persons or things that are located, gathered, or classed together.
Groups of people
* Cultural group, a group whose members share the same cultural identity
* Ethnic group, a group whose members share the same ethnic ide ...
and the stage was made in the second half of the 20th century, when stratigraphers saw the need to distinguish between
lithostratigraphic
Lithostratigraphy is a sub-discipline of stratigraphy, the geological science associated with the study of strata or rock layers. Major focuses include geochronology, comparative geology, and petrology.
In general, strata are primarily igneou ...
and
chronostratigraphic
Chronostratigraphy is the branch of stratigraphy that studies the ages of rock strata in relation to time.
The ultimate aim of chronostratigraphy is to arrange the sequence of deposition and the time of deposition of all rocks within a geologic ...
names.
Stratigraphic definition
The base of the Rupelian Stage (which is also the base of the Oligocene Series) is at the
extinction
Extinction is the termination of a kind of organism or of a group of kinds (taxon), usually a species. The moment of extinction is generally considered to be the death of the last individual of the species, although the capacity to breed and ...
of the
foraminiferan
Foraminifera (; Latin for "hole bearers"; informally called "forams") are single-celled organisms, members of a phylum or class of amoeboid protists characterized by streaming granular ectoplasm for catching food and other uses; and commonly an ...
genus
Genus ( plural genera ) is a taxonomic rank used in the biological classification of living and fossil organisms as well as viruses. In the hierarchy of biological classification, genus comes above species and below family. In binomial nom ...
''
Hantkenina
''Hantkenina'' is a genus of planktonic foraminifera that lived from the Middle Eocene up to late Eocene, cirka 49 Ma-33.9 Ma. There have been 11 morphospecies described, including one of Cribrohantkenina Coxal, H.K. y Pearson, P.N. (2006). Chapt ...
''. An official
GSSP
A Global Boundary Stratotype Section and Point (GSSP) is an internationally agreed upon reference point on a stratigraphic section which defines the lower boundary of a stage on the geologic time scale. The effort to define GSSPs is conducted ...
for the base of the Rupelian has been assigned in 1992 (
Massignano
Massignano is a ''comune'' (municipality) in the Province of Ascoli Piceno in the Italian region Marche, located about southeast of Ancona and about northeast of Ascoli Piceno. As of 31 December 2004, it had a population of 1,621 and an area of ...
, Italy). The transition with the Chattian has also been marked with a GSSP in August 2017 (
Monte Conero
Monte Conero () or Mount Conero, also known as Monte d'Ancona (Mount of Ancona), is a promontory in Italy, situated directly south of the port of Ancona on the Adriatic Sea.
The name ''Conero'' comes from the Greek name (''Kómaros'') and ind ...
, Italy).
The top of the Rupelian Stage (the base of the Chattian) is at the extinction of the foram genus ''Chiloguembelina'' (which is also the base of foram
biozone
In biostratigraphy, biostratigraphic units or biozones are intervals of geological strata that are defined on the basis of their characteristic fossil taxa, as opposed to a lithostratigraphic unit which is defined by the lithological properties ...
P21b).
The Rupelian overlaps the
Orellan
The Orellan North American Stage on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), 34-32 million years ago. It is usually considered to fall within the Early Oligocene. ...
,
Whitneyan
The Whitneyan North American Stage on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), typically set from 33,300,000 to 30,800,000 years BP, a period of . It is usuall ...
and lower
Arikareean
The Arikareean North American Stage on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), typically set from 30,600,000 to 20,800,000 years BP, a period of . It is usuall ...
North American Land Mammal Ages, the upper
Mustersan The Mustersan age is a period of geologic time (48.0–42.0 Ma) within the Eocene epoch of the Paleogene, used more specifically within the South American land mammal age (SALMA) classification. It follows the Casamayoran and precedes the Divisader ...
and
Tinguirirican The Tinguirirican ( es, Tinguiririquense) age is a period of geologic time (36.0–29.0 Ma) within the Late Eocene and Early Oligocene epochs of the Paleogene, used more specifically within the SALMA classification in South America. It follows the ...
South American Land Mammal Ages
The South American land mammal ages (SALMA) establish a geologic timescale for prehistoric South American fauna beginning 64.5 Ma during the Paleocene and continuing through to the Late Pleistocene (0.011 Ma). These periods are referred to as age ...
, the uppermost
Headonian
The Priabonian is, in the ICS's geologic timescale, the latest age or the upper stage of the Eocene Epoch or Series. It spans the time between . The Priabonian is preceded by the Bartonian and is followed by the Rupelian, the lowest stage of t ...
, Suevian and lower
Arvernian
The Arverni (Gaulish: *''Aruernoi'') were a Gallic people dwelling in the modern Auvergne region during the Iron Age and the Roman period. They were one of the most powerful tribes of ancient Gaul, contesting primacy over the region with the n ...
European Land Mammal Mega Zone
The European Land Mammal Mega Zones (abbreviation: ELMMZ, more commonly known as European land mammal ages or ELMA) are zones in rock layers that have a specific assemblage of fossils (biozones) based on occurrences of fossil assemblages of Europe ...
s (the Rupelian spans the
Mammal Paleogene zones
The Mammal Paleogene zones or MP zones are system of biostratigraphy, biostratigraphic biozone, zones in the stratigraphic record used to correlate mammal-bearing fossil localities of the Paleogene period of Europe. It consists of thirty consecutiv ...
21 through 24 and part of 25
), and the lower Hsandgolian
Asian Land Mammal Age
The Asian land mammal ages, acronym ALMA, establish a geologic timescale for prehistoric Asian fauna beginning 58.7 Mya during the Paleogene and continuing through to the Miocene ( Aquitanian) (23.03 Ma). These periods are referred to as ages, sta ...
. It is also coeval with the only regionally used upper Aldingan and lower Janjukian stages of Australia, the upper Refugian and lower Zemorrian stages of California and the lower Kiscellian
Paratethys stage of Central and eastern Europe. Other regionally used alternatives include the Stampian, Tongrian, Latdorfian and Vicksburgian.
References
Literature
* ; 1850: ''Rapport sur la carte géologique du Royaume'', Bulletins de l’Académie Royale des Sciences, des Lettres et des Beaux-Arts de Belgique 16(2), p. 351-373.
* ; 2004: ''A Geologic Time Scale 2004'',
Cambridge University Press
Cambridge University Press is the university press of the University of Cambridge. Granted letters patent by King Henry VIII in 1534, it is the oldest university press in the world. It is also the King's Printer.
Cambridge University Pre ...
.
External links
GeoWhen Database - RupelianNeogene timescale (including the upper Paleogene)an
Paleogene timescale at the website of the subcommission for stratigraphic information of the ICS
Stratigraphic chart of the Paleogene at the website of Norges Network of offshore records of geology and stratigraphy
{{Geological history, p, c
Oligocene geochronology
Geological ages