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Middle Pleistocene

Stage of the Pleistocene Epoch

Middle Pleistocene

Stage of the Pleistocene Epoch

FieldValue
nameChibanian (Middle Pleistocene)
colorChibanian
time_start0.7741
time_end0.129
image_outcropFile:Chibanian Strata.jpg
caption_outcropThe Chibanian Stratum, located at the Yoro River near Ichihara City, Japan
timelineQuaternary
name_formalityFormal
name_accept_dateJanuary 2020
synonym1Middle Pleistocene
synonym2Ionian
celestial_bodyearth
usageGlobal (ICS)
timescales_usedICS Time Scale
chrono_unitAge
strat_unitStage
timespan_formalityFormal
lower_boundary_def1.1 m below the directional midpoint of the Brunhes-Matuyama magnetic reversal
lower_gssp_locationChiba, Japan
lower_gssp_coords
lower_gssp_accept_dateJanuary 2020
upper_boundary_defNot formally defined
upper_def_candidatesMarine Isotope Substage 5e
upper_gssp_candidatesNone
The Chibanian stratum, which dates back to the Chiba period, is located along the Yoro River in Ichihara City, Chiba Prefecture. At the bottom left is a golden spike that marks the boundary between eras. The color-coded stakes on the right mark the boundaries of geological formations, indicating that the Earth's magnetic field was reversing.

The Middle Pleistocene, also known by its ICS official name of Chibanian, is an age in the international geologic timescale or a stage in chronostratigraphy, being a division of the Pleistocene Epoch within the ongoing Quaternary Period. The Chibanian name was officially ratified in January 2020. It is currently estimated to span the time between 0.7741 Ma (774,100 years ago) and 0.129 Ma (129,000 years ago), also expressed as 774.1–129 ka. It includes the transition in palaeoanthropology from the Lower to the Middle Paleolithic over 300 ka.

The Chibanian is preceded by the Calabrian and succeeded by the Late Pleistocene. The beginning of the Chibanian is the Brunhes–Matuyama reversal, when the Earth's magnetic field last underwent reversal. Its end roughly coincides with the termination of the Penultimate Glacial Period and the onset of the Last Interglacial period (corresponding to the beginning of Marine Isotope Stage 5).

The term Middle Pleistocene was in use as a provisional or "quasi-formal" designation by the International Union of Geological Sciences (IUGS). While the three lowest ages of the Pleistocene, the Gelasian, Calabrian and Chibanian have been officially defined, the Late Pleistocene has yet to be formally defined.

Definition process

The International Union of Geological Sciences (IUGS) had previously proposed replacement of the Middle Pleistocene by an Ionian Age based on strata found in Italy. In November 2017, however, the Chibanian (based on strata at a site in Chiba Prefecture, Japan) replaced the Ionian as the Subcommission on Quaternary Stratigraphy's preferred GSSP proposal for the age that should replace the Middle Pleistocene sub-epoch. The "Chibanian" name was ratified by the IUGS in January 2020.

Climate

By early Middle Pleistocene, the Mid-Pleistocene Transition had changed the glacial cycles from an average 41,000 year periodicity present during most of the Early Pleistocene to a 100,000 year periodicity, with the glacial cycles becoming asymmetric, having long glacial periods punctuated by short warm interglacial periods. Millennial-scale climatic variability continued to be highly sensitive to precession and obliquity cycles.

In central Italy, the climate became noticeably more arid from 600 ka to 400 ka.

The late Middle Pleistocene was a time of regional aridification in the Levant, with a shallow lake covering what is now the Shishan Marsh drying and developing into a marsh.

Eastern Africa's hydroclimate was governed primarily by orbital precession, although modulated significantly by the 100 kyr eccentricity cycle.

Along the northwestern Australian coast, the intensification of the Leeuwin Current resulted in an expansion of reefs coincident with the Great Barrier Reef's formation.

Events

The Early-Middle Pleistocene boundary saw the migration of true horses out of North America and into Eurasia. Also around this time, the European mammoth species Mammuthus meridionalis became extinct and was replaced by the Asian species Mammuthus trogontherii (the steppe mammoth). This was coincident with the migration of the elephant genus Palaeoloxodon out of Africa and into Eurasia, including the first appearance of species like the European straight-tusked elephant (Palaeoloxodon antiquus). With the extinction of Sinomastodon in East Asia at the Early-Middle Pleistocene boundary, gomphotheres became completely extinct in Afro-Eurasia, but continued to persist in the Americas into the Late Pleistocene. There was a major extinction of carnivorous mammals in Europe around the Early-Middle Pleistocene transition, including the giant hyena Pachycrocuta. The mid-late Middle Pleistocene saw the emergence of the woolly mammoth (Mammuthus primigenius), and its replacement of Mammuthus trogontherii, with the replacement of M. trogontherii in Europe by woolly mammoths being complete by around 200,000 years ago. The last member of the notoungulate family Mesotheriidae, Mesotherium, has its last records around 220,000 years ago, leaving Toxodontidae as the sole family of notoungulates to persist into the Late Pleistocene. During the late Middle Pleistocene, around 195,000–135,000 years ago, the steppe bison (the ancestor of the modern American bison) migrated across the Bering land bridge into North America, marking the beginning of the Rancholabrean faunal stage. Around 500,000 years ago, the last members of the largely European aquatic frog genus Palaeobatrachus and by extension the family Palaeobatrachidae became extinct.

Palaeoanthropology

The Chibanian includes the transition in palaeoanthropology from the Lower to the Middle Paleolithic: i.e., the emergence of Homo sapiens sapiens between 300 ka and 400 ka. The oldest known human DNA dates to the Middle Pleistocene, around 430,000 years ago. This is the oldest found, .

After analyzing 2,496 remains of Castor fiber (Eurasian beaver) and Trogontherium cuvieri found at Bilzingsleben in Germany, a team of scientists concluded that, around 400 ka, hominids in the area hunted and exploited beavers. They may have been targeted for their meat (based on cut marks on the bones) and skin.

Chronology

Agepaleoclimateglaciationpalaeoanthropology
790–761 kaMIS 19Günz (Elbe) glaciationPeking Man (Homo erectus)
761–712 kaMIS 18
712–676 kaMIS 17
676–621 kaMIS 16
621–563 kaMIS 15Gunz-Haslach interglacialHeidelberg Man (Homo heidelbergensis), Bodo cranium
563–524 kaMIS 14
524–474 kaMIS 13end of Cromerian (Günz-Mindel) interglacialBoxgrove Man (Homo heidelbergensis)
474–424 kaMIS 12Anglian Stage in Britain; Haslach glaciationTautavel Man (Homo erectus)
424–374 kaMIS 11Hoxnian (Britain), Yarmouthian (North America)Swanscombe Man (Homo heidelbergensis)
374–337 kaMIS 10Mindel glaciation, Elster glaciation, Riss glaciation
337–300 kaMIS 9Purfleet Interglacial in BritainMousterian
300–243 kaMIS 8Irhoud 1 (Homo sapiens); Middle Paleolithic; Haplogroup A (Y-DNA)
243–191 kaMIS 7Aveley Interglacial in BritainGalilee Man; Haua Fteah
191–130 kaMIS 6Illinoian StageHerto Man (Homo sapiens); Macro-haplogroup L (mtDNA); Mousterian
130–123 kaMIS 5epeak of Eemian interglacial sub-stage, or Ipswichian in BritainKlasies River Caves; Sangoan

References

References

  1. "Global Boundary Stratotype Section and Point". International Commission of Stratigraphy.
  2. Hornyak, Tim. (30 January 2020). "Japan Puts Its Mark on Geologic Time with the Chibanian Age". [[American Geophysical Union]].
  3. "Global Boundary Stratotype Section and Points".
  4. (2004). "A Geological Time Scale 2004". Cambridge University Press.
  5. D. Dahl-Jensen & others. (2013). "Eemian interglacial reconstructed from a Greenland folded ice core". Nature.
  6. P. L. Gibbard. (17 April 2015). "The Quaternary System/Period and its major sub-divisions". Elsevier BV.
  7. (14 November 2017). "Japan-based name 'Chibanian' set to represent geologic age of last magnetic shift". The Japan Times.
  8. (June 2021). "On the Cause of the Mid-Pleistocene Transition". Reviews of Geophysics.
  9. (2017-12-12). "Causes of ice age intensification across the Mid-Pleistocene Transition". Proceedings of the National Academy of Sciences.
  10. (1 November 2021). "Persistent orbital influence on millennial climate variability through the Pleistocene". [[Nature Geoscience]].
  11. (10 May 2022). "Middle Pleistocene paleoclimate and paleoenvironment of central Italy and their relationship with hominin migrations and evolution". [[Quaternary International]].
  12. (1 June 2022). "The Middle to Late Pleistocene transition in the Azraq Oasis, Jordan: A phytolith-based reconstruction of wetland palaeoecology". [[Palaeogeography, Palaeoclimatology, Palaeoecology]].
  13. (24 February 2022). "Orbital controls on eastern African hydroclimate in the Pleistocene". [[Scientific Reports]].
  14. (November 2014). "Seismic and stratigraphic evidence for reef expansion and onset of aridity on the Northwest Shelf of Australia during the Pleistocene". [[Marine and Petroleum Geology]].
  15. (December 2021). "Ancient horse genomes reveal the timing and extent of dispersals across the Bering Land Bridge". Molecular Ecology.
  16. Lister, Adrian M.. (2004). "Human Paleoecology in the Levantine Corridor". Oxbow Books.
  17. (August 2014). "New remains of Sinomastodon yangziensis (Proboscidea, Gomphotheriidae) from Sanhe karst Cave, with discussion on the evolution of Pleistocene Sinomastodon in South China". Quaternary International.
  18. (1 July 2021). "The rise and fall of proboscidean ecological diversity". Nature Ecology & Evolution.
  19. (March 2008). "Carnivora dispersal in Western Mediterranean during the last 2.6Ma". Quaternary International.
  20. Lister, Adrian M.. (October 2022). "Mammoth evolution in the late Middle Pleistocene: The Mammuthus trogontherii-primigenius transition in Europe". Quaternary Science Reviews.
  21. (February 2023). "The last record of the last typotherid (Notoungulata, Mesotheriidae, Mesotherium cristatum) for the middle Pleistocene of the western Pampean region, Córdoba Province, Argentina, and its biostratigraphic implications". Quaternary Science Reviews.
  22. (2017-03-28). "Fossil and genomic evidence constrains the timing of bison arrival in North America". Proceedings of the National Academy of Sciences.
  23. (September 2012). "Generic diversity and distributional dynamics of the Palaeobatrachidae (Amphibia: Anura)". Palaeobiodiversity and Palaeoenvironments.
  24. D. Richter & others. (8 June 2017). "The Age of Hominin Fossils from Jebel Irhoud, Morocco, and the origins of the Middle Stone Age". Nature.
  25. Crew, Bec. (15 March 2016). "The Oldest Human Genome Ever Has Been Sequenced, And It Could Rewrite Our History". ScienceAlert.
  26. (2023-11-13). "Beaver exploitation, 400,000 years ago, testifies to prey choice diversity of Middle Pleistocene hominins". Scientific Reports.
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