| |  Online-Ressource |
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| Verfasst von: | Hering, Fabio [VerfasserIn]  |
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| | Stinnesbeck, Wolfgang [VerfasserIn] |
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| | Folmeister, Jens [VerfasserIn] |
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| | Frey, Eberhard [VerfasserIn] |
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| | Stinnesbeck, Sarah [VerfasserIn] |
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| | Avilés, Jerónimo [VerfasserIn] |
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| | Núñez, Eugenio Aceves [VerfasserIn] |
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| | González, Arturo [VerfasserIn] |
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| | Terrazas Mata, Alejandro [VerfasserIn] |
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| | Benavente, Martha Elena [VerfasserIn] |
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| | Rojas, Carmen [VerfasserIn] |
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| | Velázquez Morlet, Adriana [VerfasserIn] |
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| | Frank, Norbert [VerfasserIn] |
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| | Zell, Patrick [VerfasserIn] |
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| | Becker, Julia [VerfasserIn] |
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| Titel: | The Chan Hol cave near Tulum (Quintana Roo, Mexico) |
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| Titelzusatz: | evidence for long-lasting human presence during the early to middle Holocene |
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| Verf.angabe: | Fabio Hering, Wolfgang Stinnesbeck, Jens Folmeister, Eberhard Frey, Sarah Stinnesbeck, Jerónimo Avilés, Eugenio Aceves Núñez, Arturo González, Alejandro Terrazas Mata, Martha Elena Benavente, Carmen Rojas, Adriana Velázquez Morlet, Norbert Frank, Patrick Zell, Julia Becker |
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| E-Jahr: | 2018 |
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| Jahr: | 17 April 2018 |
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| Umfang: | 11 S. |
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| Teil: | volume:33 |
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| | year:2018 |
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| | number:4 |
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| | pages:444-454 |
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| | extent:11 |
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| Fussnoten: | First published: 17 April 2018 ; Gesehen am 18.12.2019 |
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| Titel Quelle: | Enthalten in: Journal of quaternary science |
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| Ort Quelle: | New York, NY [u.a.] : Wiley, 1986 |
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| Jahr Quelle: | 2018 |
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| Band/Heft Quelle: | 33(2018), 4, Seite 444-454 |
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| ISSN Quelle: | 1099-1417 |
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| Abstract: | Numerous charcoal accumulations discovered in the submerged Chan Hol cave near Tulum, Quintana Roo, Mexico, have been 14C-dated revealing ages between 8110 ± 28 14C a BP (9122-8999 cal a BP) and 7177 ± 27 14C a BP (8027-7951 cal a BP). These charcoal concentrations, interpreted here as ancient illumination sites, provide strong evidence that the Chan Hol cave was dry and accessible during that time interval. Humans used the cave for at least 1200 years during the early and middle Holocene, before access was successively interrupted by global sea level rise and flooding of the cave system. Our data thus narrow the gap between an early settlement in the Tulum area reaching from the late Pleistocene (∼13 000 a) to middle Holocene (e.g. 7177 14C a BP), and the Maya Formative period at approximately 3000 a bp. Yet, no evidence has been presented to date for human settlement during the ∼4000-year interval between 7000 and 3000 a. This is remarkable as settlement in other areas of south-eastern Mexico (e.g. Chiapas, Tabasco) and in Guatemala was apparently continuous. |
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| DOI: | doi:10.1002/jqs.3025 |
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| URL: | Bitte beachten Sie: Dies ist ein Bibliographieeintrag. Ein Volltextzugriff für Mitglieder der Universität besteht hier nur, falls für die entsprechende Zeitschrift/den entsprechenden Sammelband ein Abonnement besteht oder es sich um einen OpenAccess-Titel handelt.
Volltext ; Verlag: https://doi.org/10.1002/jqs.3025 |
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| | Volltext: https://onlinelibrary.wiley.com/doi/abs/10.1002/jqs.3025 |
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| | DOI: https://doi.org/10.1002/jqs.3025 |
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| Datenträger: | Online-Ressource |
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| Sprache: | eng |
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| Sach-SW: | Charcoal |
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| | Early Holocene |
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| | Human settlement |
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| | Pre-Maya settlement |
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| | Sea level rise |
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| | Submerged cave |
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| | Yucatán Peninsula |
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| K10plus-PPN: | 1685941168 |
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| Verknüpfungen: | → Zeitschrift |
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¬The¬ Chan Hol cave near Tulum (Quintana Roo, Mexico) / Hering, Fabio [VerfasserIn]; 17 April 2018 (Online-Ressource)
