DOI: 10.1016/j.quascirev.2013.09.009
Scopus记录号: 2-s2.0-84886247737
论文题名: Rethinking stratigraphy and site formation of the Pleistocene deposit at Cueva Negra del Estrecho del Río Quípar (Caravaca de la Cruz, Spain)
作者: Angelucci D.E. ; Anesin D. ; López Martínez M. ; Haber Uriarte M. ; Rodríguez Estrella T. ; Walker M.J.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2013
卷: 80 起始页码: 195
结束页码: 199
语种: 英语
英文关键词: Alluvial sediment
; Early Pleistocene
; Geoarchaeology
; Rock-shelter
Scopus关键词: Alluvial sediments
; Early pleistocene
; Field observations
; Geo archaeologies
; Information-on site
; Pleistocene deposits
; Rock-shelter
; Thermal alteration
; Geomagnetism
; Stratigraphy
; Deposits
; alluvial deposit
; anthropogenic effect
; archaeology
; cave
; depositional environment
; displacement
; excavation
; faunistics
; Holocene
; lithic fragment
; micromorphology
; paleomagnetism
; Pleistocene
; stratigraphy
; tooth
; Cueva Negra del Estrecho del Rio Quipar
; Murcia [Spain]
; Spain
英文摘要: Cueva Negra del Estrecho del Río Quípar (Caravaca de la Cruz, Murcia, Spain), hereinafter Cueva Negra, is a key-site for understanding the early peopling of Europe. Since 1990, systematic excavation has revealed an intriguing assemblage of lithic and faunal remains, and hominin teeth. It was deposited 0.99-0.78Ma according to palaeomagnetic and biostratigraphical data; pollen data indicate warm moist conditions. Recently, possible evidence of thermal alteration was detected in a deep part of the deposit. We report here on our revision of the Cueva Negra stratigraphy, and offer information on site formation processes, based on new field observations and preliminary data from soil micromorphology. The Cueva Negra succession comprises three main stratigraphical complexes. Complex 1 is late Holocene. Complexes 2 and 3 are Pleistocene and are formed mainly of alluvial sediment, with subordinate inputs from the cave walls. Complexes 2 and 3 were accumulated almost without interruption, being separated by an erosive surface truncating a thin alluvial soil developed at the top of Complex 3. Our initial micromorphological findings indicate that anthropic inputs are mostly in derived positions, very likely having undergone inward displacement from the mouth of the rock-shelter. © 2013 Elsevier Ltd. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/60468
Appears in Collections: 过去全球变化的重建
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作者单位: Dipartimento di Lettere e Filosofia, Università di Trento, via T. Gar 14, I-38122 Trento, Italy; Área de Antropología Física, Departamento de Zoología y Antropología Física, Universidad de Murcia, Spain; Área de Prehistoria, Dep. de Prehistoria, Arqueologia, Historia Antigua, Historia Medieval y Ciencias y Tecnicas Historiograficas, Universidad de Murcia, Spain; Escuela de Ingeniería Minera, Geológica y Cartográfica, Universidad Politécnica de Cartagena, Spain
Recommended Citation:
Angelucci D.E.,Anesin D.,López Martínez M.,et al. Rethinking stratigraphy and site formation of the Pleistocene deposit at Cueva Negra del Estrecho del Río Quípar (Caravaca de la Cruz, Spain)[J]. Quaternary Science Reviews,2013-01-01,80