干旱区生态环境知识资源中心(Arid): The Middle to Late Pleistocene herpetofaunal assemblages from the Jarama and Manzanares valleys (Madrid, central Spain): An ecological synthesis

Arid

DOI	10.1016/j.quaint.2018.03.004
	The Middle to Late Pleistocene herpetofaunal assemblages from the Jarama and Manzanares valleys (Madrid, central Spain): An ecological synthesis
	Blain, Hugues-Alexandre; Bisbal-Chinesta, Josep Francesc; Martinez-Monzon, Almudena; Panera, Joaquin; Rubio-Jara, Susana; Uribelarrea, David; Sainz de los Terreros, Jose Yravedra; Perez-Gonzalez, Alfredo
通讯作者	Blain, HA (corresponding author), Inst Catala Paleoecol Humana & Evolucio Social, IPHES, Zona Educac 4,Campus Sescelades URV Edif W3, Tarragona 43007, Spain.
来源期刊	QUATERNARY INTERNATIONAL
ISSN	1040-6182
EISSN	1873-4553
出版年	2019
卷号	520 页码:49-63
英文摘要	The successive fossil amphibian and reptile assemblages from the Middle to Late Pleistocene sites from the Manzanares and Jarama River Valleys (Madrid, central Spain) permitted the reconstruction of part of the climate instability with high-amplitude and rapid shifts of the last 450 ka and their associated landscapes: Aridos-1 (MIS11b), Valdocarros II (MIS8a/7e), Estanque de Tormentas de Butarque ETB-H02 (MIS7d or MIS6), PRERESA (MIS7/6 or MIS5a) and HAT (MIS5a). This work aims to present a regional synthesis of the palaeoclimatic and palaeoenvironmental data obtained from the herpetofaunal assemblages for these two valleys and their influence on the biodiversity during the Pleistocene. As a whole, these archaeo-paleontological localities document a total of 20 taxa (8 anurans and 12 reptiles) thus representing 76.9% of the modern authochtonous herpetofauna of the southeast of the Region of Madrid. Taking as a reference the modern situation in the area, the successive herpetofaunal assemblages permits a hypothetical landscape reconstruction where three different periods are represented with a glacial landscape (ETB-H02), a landscape of transition from cool to temperate climatic conditions (Valdocarros II), and an interglacial landscape (Aridos-1, HAT, PRERESA, and today). Environment is particularly open during dry periods, independently of if it is cold or warm. The main difference between an interglacial and a glacial period is the opposite representation of woodlands vs. moist environments: the last ones being more represented during cold periods than during warm periods. Finally, as documented by the succession from Valdocarros II, periods of transition between cold and warm climate are more forested but at the expense of humid meadows progressively. According to the relation between richness, biodiversity and climatic and environmental factors, a clear correlation appears between reptile richness and woodlands. In a similar way, mean annual precipitation (MAP) is revealed to be the most influent factor on reptile local diversity certainly because of its implications on vegetal cover extension and ecosystem productivity and resources. For amphibians the MAP does not influence dominancy but species richness: anuran richness being higher for lower MAP. Such an unusual pattern is certainly due to the fact that there are no strict forest-dweller anurans within the archaeological assemblages and that most of the anurans present in the sites are well adapted to arid conditions. (C) 2018 Elsevier Ltd and INQUA. All rights reserved.
英文关键词	Middle and Late Pleistocene Cold to warm climate Terrestrial environments Amphibians Reptiles Central Iberian peninsula
类型	Article
语种	英语
收录类别	SCI-E ; SSCI
WOS记录号	WOS:000502532700005
WOS关键词	CENTRAL IBERIAN PENINSULA ; ISOTOPE STAGE 11 ; MICROHABITAT SELECTION ; CLIMATE VARIABILITY ; TENAGHI-PHILIPPON ; SQUAMATE REPTILE ; VEGETATION ; LIZARD ; RECORD ; SEQUENCE
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向	Physical Geography ; Geology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/369318
作者单位	[Blain, Hugues-Alexandre; Bisbal-Chinesta, Josep Francesc; Martinez-Monzon, Almudena] Inst Catala Paleoecol Humana & Evolucio Social, IPHES, Zona Educac 4,Campus Sescelades URV Edif W3, Tarragona 43007, Spain; [Blain, Hugues-Alexandre; Bisbal-Chinesta, Josep Francesc; Martinez-Monzon, Almudena] URV, Area Prehist, Avinguda Catalunya 35, Tarragona 43002, Spain; [Panera, Joaquin; Rubio-Jara, Susana; Perez-Gonzalez, Alfredo] Ctr Nacl Invest Evoluc Humana, CENIEH, Paseo Sierra Atapuerca 3, Burgos 09002, Spain; [Uribelarrea, David] Univ Complutense Madrid, Fac Ciencias Geol, Dept Geodinam, C Jose Antonio Novais 2, E-28040 Madrid, Spain; [Sainz de los Terreros, Jose Yravedra] Univ Complutense Madrid, Dept Prehist, C Prof Aranguren S-N, E-28040 Madrid, Spain
推荐引用方式 GB/T 7714	Blain, Hugues-Alexandre,Bisbal-Chinesta, Josep Francesc,Martinez-Monzon, Almudena,et al. The Middle to Late Pleistocene herpetofaunal assemblages from the Jarama and Manzanares valleys (Madrid, central Spain): An ecological synthesis[J],2019,520:49-63.
APA	Blain, Hugues-Alexandre.,Bisbal-Chinesta, Josep Francesc.,Martinez-Monzon, Almudena.,Panera, Joaquin.,Rubio-Jara, Susana.,...&Perez-Gonzalez, Alfredo.(2019).The Middle to Late Pleistocene herpetofaunal assemblages from the Jarama and Manzanares valleys (Madrid, central Spain): An ecological synthesis.QUATERNARY INTERNATIONAL,520,49-63.
MLA	Blain, Hugues-Alexandre,et al."The Middle to Late Pleistocene herpetofaunal assemblages from the Jarama and Manzanares valleys (Madrid, central Spain): An ecological synthesis".QUATERNARY INTERNATIONAL 520(2019):49-63.