Published April 8, 2026
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TABLE 2 in How depositional environments impact the preservation of micro-wear of quartz artifacts: insights from the Oldowan of the Shungura Formation (Ethiopia)
Authors/Creators
- 1. Pleistocene Archaeology Lab, Instituto de Historia, Spanish National Research Council (CSIC), Calle de Albasanz, 26, San Blas-Canillejas, Madrid 28037 (Spain) and De la Préhistoire à l'Actuel: Culture, Environnement et Anthropologie (PACEA), Université de Bordeaux, CNRS, Bâtiment B 2, Allée Geoffroy Saint-Hilaire CS 50023, 33615 Pessac (France) aline. galland @ u-bordeaux. fr (corresponding autor)
- 2. Institució milà i fontanals de estudios en humanidades (IMF), Spanish National Research Council (CSIC), Carrer de les Egipcíaques, 15, 08001, Barcelona (Spain) ignacio @ imf. csic. es
- 3. French Centre for Ethiopian Studies (CFEE), CNRS, Ministry of Europe and Foreign Affairs, Arada sub city, Kebele 11 / 12, JanMeda, PO BOX 5554 Addis Ababa (Ethiopia) and Laboratory Paleontology Evolution Paleoecosystems Paleoprimatology (PALEVOPRIM), CNRS, Université de Poitiers, 6 Rue Michel Brunet, 86000 Poitiers (France) jean. renaud. boisserie @ univ-poitiers. fr
- 4. De la Préhistoire à l'Actuel: Culture, Environnement et Anthropologie (PACEA), Université de Bordeaux, CNRS, Bâtiment B 2, Allée Geoffroy Saint-Hilaire CS 50023, 33615 Pessac (France) anne. delagnes @ u-bordeaux. fr
Description
TABLE 2. — Synthesis of taphonomic microwear types and their relative abundance,comparing experiments and the depositional environments in the archaeological record. The scale indicates the degree of development of each microwear category: (-) not observed or only present as highly localized traces, and relative abundance (+, present; ++, abundant; +++, very abundant).
| Context | Striation | Microwear Scarring Rounding Microfracturing | Polish | ||
|---|---|---|---|---|---|
| Fluvial transport_Sand | - | + | +++ | +++ | - |
| Fluvial transport_Silt | - | - | +++ | +++ | - |
| Fluvial transport_Clay | - | - | +++ | + | +++ |
| Aeolian abrasion (1min) | - | + | - | - | - |
| Aeolian abrasion (5min) | - | ++ | - | +++ | - |
| Channel lags | - | ++ | ++ | +++ | - |
| Point bar | - | + | + | ++ | - |
| Floodplain | - | ++ | ++ | +++ | ++ |
Notes
Published as part of Galland, Aline, Clemente-Conte, Ignacio, Boisserie, Jean-Renaud & Delagnes, Anne, 2026, How depositional environments impact the preservation of micro-wear of quartz artifacts: insights from the Oldowan of the Shungura Formation (Ethiopia), pp. 113 in Comptes Rendus Palevol 25 (6) on page 113, DOI: 10.5852/cr-palevol2026v25a6, http://zenodo.org/record/19700687
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- Is part of
- Journal article: 10.5852/cr-palevol2026v25a6 (DOI)
- Journal article: urn:lsid:plazi.org:pub:28148215FF91FFDAFFFEFFBC737A5869 (LSID)
- Journal article: http://zenodo.org/record/19700687 (URL)
- Journal article: http://publication.plazi.org/id/28148215FF91FFDAFFFEFFBC737A5869 (URL)
- Journal article: http://zoobank.org/urn:lsid:zoobank.org:pub:415FDDE5-4CF5-4F9D-BF34-5CFB1E6ABEE1 (URL)