About: Early Pleistocene   Sponge Permalink

An Entity of Type : owl:Thing, within Data Space : 134.155.108.49:8890 associated with source dataset(s)

Early Pleistocene (also known as Lower Pleistocene, or Calabrian) is a subdivision of the Pleistocene Epoch of the Geologic time scale. The beginning of the stage is defined at 1.806 ± 0.005 Ma (million years ago). The end of the stage is defined by the last magnetic pole reversal 781,000 ± 5,000 years ago. Originally the Calabrian was a European faunal stage primarily based on mollusk fossils. It has been subsumed into, and become equivalent to, the geologic stage called the Early Pleistocene. However, many of the mammalian faunal assemblages of the Early Pleistocene start in the Gelasian (last stage of the Pliocene). For example, the Platygonus and other Blancan fauna appear first in the Gelasian.

AttributesValues
rdfs:label
  • Early Pleistocene
rdfs:comment
  • Early Pleistocene (also known as Lower Pleistocene, or Calabrian) is a subdivision of the Pleistocene Epoch of the Geologic time scale. The beginning of the stage is defined at 1.806 ± 0.005 Ma (million years ago). The end of the stage is defined by the last magnetic pole reversal 781,000 ± 5,000 years ago. Originally the Calabrian was a European faunal stage primarily based on mollusk fossils. It has been subsumed into, and become equivalent to, the geologic stage called the Early Pleistocene. However, many of the mammalian faunal assemblages of the Early Pleistocene start in the Gelasian (last stage of the Pliocene). For example, the Platygonus and other Blancan fauna appear first in the Gelasian.
sameAs
dcterms:subject
dbkwik:fossil/prop...iPageUsesTemplate
abstract
  • Early Pleistocene (also known as Lower Pleistocene, or Calabrian) is a subdivision of the Pleistocene Epoch of the Geologic time scale. The beginning of the stage is defined at 1.806 ± 0.005 Ma (million years ago). The end of the stage is defined by the last magnetic pole reversal 781,000 ± 5,000 years ago. Originally the Calabrian was a European faunal stage primarily based on mollusk fossils. It has been subsumed into, and become equivalent to, the geologic stage called the Early Pleistocene. However, many of the mammalian faunal assemblages of the Early Pleistocene start in the Gelasian (last stage of the Pliocene). For example, the Platygonus and other Blancan fauna appear first in the Gelasian.
Alternative Linked Data Views: ODE     Raw Data in: CXML | CSV | RDF ( N-Triples N3/Turtle JSON XML ) | OData ( Atom JSON ) | Microdata ( JSON HTML) | JSON-LD    About   
This material is Open Knowledge   W3C Semantic Web Technology [RDF Data] Valid XHTML + RDFa
OpenLink Virtuoso version 07.20.3217, on Linux (x86_64-pc-linux-gnu), Standard Edition
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2012 OpenLink Software