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Calabrian (stage) facts for kids

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1.80 – 0.774 Ma
Quaternary graphical timeline
-2.6 —
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-1 —
-0.8 —
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Subdivision of the Quaternary according to the ICS, as of 2021.
Vertical axis scale: millions of years ago.
Name formality Formal
Usage information
Celestial body Earth
Regional usage Global (ICS)
Time scale(s) used ICS Time Scale
Chronological unit Age
Stratigraphic unit Stage
Time span formality Formal
Lower boundary definition Approximately 8 m after the end of magnetic polarity chronozone C2n (Olduvai)
Lower boundary GSSP Vrica Section, Calabria, Italy
39°02′19″N 17°08′05″E / 39.0385°N 17.1348°E / 39.0385; 17.1348
Lower GSSP ratified 5 December 2011 (as base of Calabrian)
Upper boundary definition 1.1 m below the directional midpoint of the Brunhes-Matuyama magnetic reversal
Upper boundary GSSP Chiba, Japan
35°17′39″N 140°08′47″E / 35.2943°N 140.1465°E / 35.2943; 140.1465
Upper GSSP ratified 2020

Calabrian is a subdivision of the Pleistocene Epoch of the geologic time scale, defined as 1.8 Ma—774,000 years ago ± 5,000 years, a period of ~1.026 million years.

The end of the stage is defined by the last magnetic pole reversal (781 ± 5 Ka) and plunge into an ice age and global drying possibly colder and drier than the late Miocene (Messinian) through early Pliocene (Zanclean) cold period. Originally the Calabrian was a European faunal stage primarily based on mollusk fossils. It has become the second geologic age in the Early Pleistocene. Many of the mammalian faunal assemblages of the Early Pleistocene start in the Gelasian. For example, the Platygonus and other Blancan fauna appear first in the Gelasian.

History of the definition of the Calabrian

Because sea shells are much more abundant as fossils, 19th- and early-20th-century geo-scientists used the plentiful and well-differentiatable Mollusca (mollusks) and Brachiopods to identify stratigraphic boundaries. Thus the Calabrian was originally defined as an assemblage of mollusk fossils, most brachiopods being extinct by then. Efforts were then made to find the best representation of that assemblage in a stratigraphic section. By 1948 scientists used the initial appearance of cool-water (northern) invertebrate faunas in Mediterranean marine sediments as the beginning marker for the Calabrian. The 18th International Geological Congress in London (1948) placed the base of the Pleistocene at the base of the marine strata of the Calabrian Faunal Stage and denominated a type section in southern Italy. However, it was discovered that the original type section was discontinuous at that point and that the base of the Calabrian Stage as defined by fauna assemblages extended to earlier levels within the Pleistocene. A new type section was chosen, several miles from the original one, at Vrica, 4 km south of Crotone in Calabria, southern Italy. Analysis of strontium and oxygen isotopes as well as of planktonic foraminifera has confirmed the viability of the current type section. The 27th International Geological Congress in Moscow in 1984 formally ratified the type section. The starting date was originally thought to be about 1.65 million years ago, but has been recalculated as 1.806 Mya.

Present formal definition

The Global Boundary Stratotype Section and Point, GSSP, for the former start of the Pleistocene is in a reference section at Vrica, 4 km south of Crotone in Calabria, Southern Italy, a location whose exact dating has recently been confirmed by analysis of strontium and oxygen isotopes as well as by planktonic foraminifera.

The beginning of the Calabrian hence is defined as: Just above top of magnetic polarity chronozone C2n (Olduvai) and the extinction level of calcareous nannofossil Discoaster brouweri (base Zone CN13). Above the boundary are the lowest occurrence of calcareous nannofossil medium Gephyrocapsa spp. and the extinction level of the planktonic foraminifer Globigerinoides extremus.

The end of the Calabrian is defined as the Brunhes–Matuyama magnetic reversal event.

See also

Kids robot.svg In Spanish: Calabriense para niños

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