FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2189607413> ?p ?o ?g. }

• W2189607413 endingPage "32" @default.
• W2189607413 startingPage "20" @default.
• W2189607413 abstract "The major social and economic changes associated with the rise of a sedentary lifestyle and the gradual transition to food production in the southern Levant are often considered to have been triggered by climate changes at the end of the Pleistocene (∼20,000–11,000 years BP). This explanation, however, is biased by the scarcity of high-resolution climate records directly associated with human activity and the lack of refined palaeoecological studies from multi-stratified sites in the area. Here, we present the results of an anthracological analysis, carried out on charcoals collected along a continuous column of archaeological sediments in the Natufian site of el-Wad Terrace (Mount Carmel, Israel). We also present the carbon isotopes analysis of 14C-dated archaeological remains of Amygdalus sp. The analyses of charcoal shows the predominance of an oak forest including Quercus calliprinos and ithaburensis around the site during the Early Natufian building phase (∼14,600–13,700 cal BP), and the values of Δ13C point to a high rainfall rate. This period is followed by a marked decrease in the local rainfall between ∼13,700 and 12,000 cal BP). The reduction, culturally associated with the latest Early Natufian and the Late Natufian, is independently recorded by the speleothems of the region: Soreq Cave and Jerusalem Cave. This period incorporates an increase in drought tolerant species such as Amygdalus sp. Thermo-Mediterranean species, such as Olea europaea and Ceratonia siliqua, as well as Pistacia palaestina, which dominate the modern landscape, become established in the Holocene. We conclude that the Natufian settlement at el-Wad Terrace flourished in the context of oak forests, and subsequently occupation intensity decreased in concurrence to the drying trend. This shift does not correspond to the cultural typology (i.e. Early Natufian vs. Late Natufian). Human response to climate change at the terminal Pleistocene Levant was multifaceted and localized. Its understanding requires the analysis of records that are well-tied to human ecology and behavior." @default.
• W2189607413 created "2016-06-24" @default.
• W2189607413 creator A5005644878 @default.
• W2189607413 creator A5013360117 @default.
• W2189607413 creator A5032863801 @default.
• W2189607413 creator A5043367352 @default.
• W2189607413 creator A5048243538 @default.
• W2189607413 creator A5048825165 @default.
• W2189607413 date "2016-01-01" @default.
• W2189607413 modified "2023-09-26" @default.
• W2189607413 title "Charred wood remains in the natufian sequence of el-Wad terrace (Israel): New insights into the climatic, environmental and cultural changes at the end of the Pleistocene" @default.
• W2189607413 cites W1521025934 @default.
• W2189607413 cites W1837907234 @default.
• W2189607413 cites W1839041501 @default.
• W2189607413 cites W1867019107 @default.
• W2189607413 cites W1875494317 @default.
• W2189607413 cites W1926764738 @default.
• W2189607413 cites W1965672898 @default.
• W2189607413 cites W1982075842 @default.
• W2189607413 cites W1988343654 @default.
• W2189607413 cites W1994563382 @default.
• W2189607413 cites W2000375557 @default.
• W2189607413 cites W2002081351 @default.
• W2189607413 cites W2004295103 @default.
• W2189607413 cites W2004584508 @default.
• W2189607413 cites W2009810898 @default.
• W2189607413 cites W2012068109 @default.
• W2189607413 cites W2014502866 @default.
• W2189607413 cites W2024151663 @default.
• W2189607413 cites W2031621566 @default.
• W2189607413 cites W2042862378 @default.
• W2189607413 cites W2043714934 @default.
• W2189607413 cites W2046373624 @default.
• W2189607413 cites W2051433456 @default.
• W2189607413 cites W2052942492 @default.
• W2189607413 cites W2059014184 @default.
• W2189607413 cites W2060800393 @default.
• W2189607413 cites W2062362890 @default.
• W2189607413 cites W2067817745 @default.
• W2189607413 cites W2076896609 @default.
• W2189607413 cites W2080355489 @default.
• W2189607413 cites W2092805412 @default.
• W2189607413 cites W2094483372 @default.
• W2189607413 cites W2095648000 @default.
• W2189607413 cites W2113817995 @default.
• W2189607413 cites W2123849736 @default.
• W2189607413 cites W2126150941 @default.
• W2189607413 cites W2126964894 @default.
• W2189607413 cites W2141888613 @default.
• W2189607413 cites W2142208875 @default.
• W2189607413 cites W2143804637 @default.
• W2189607413 cites W2148343009 @default.
• W2189607413 cites W2158535443 @default.
• W2189607413 cites W2163734833 @default.
• W2189607413 cites W2332898923 @default.
• W2189607413 doi "https://doi.org/10.1016/j.quascirev.2015.10.034" @default.
• W2189607413 hasPublicationYear "2016" @default.
• W2189607413 type Work @default.
• W2189607413 sameAs 2189607413 @default.
• W2189607413 citedByCount "30" @default.
• W2189607413 countsByYear W21896074132016 @default.
• W2189607413 countsByYear W21896074132017 @default.
• W2189607413 countsByYear W21896074132018 @default.
• W2189607413 countsByYear W21896074132019 @default.
• W2189607413 countsByYear W21896074132020 @default.
• W2189607413 countsByYear W21896074132021 @default.
• W2189607413 countsByYear W21896074132022 @default.
• W2189607413 countsByYear W21896074132023 @default.
• W2189607413 crossrefType "journal-article" @default.
• W2189607413 hasAuthorship W2189607413A5005644878 @default.
• W2189607413 hasAuthorship W2189607413A5013360117 @default.
• W2189607413 hasAuthorship W2189607413A5032863801 @default.
• W2189607413 hasAuthorship W2189607413A5043367352 @default.
• W2189607413 hasAuthorship W2189607413A5048243538 @default.
• W2189607413 hasAuthorship W2189607413A5048825165 @default.
• W2189607413 hasConcept C100970517 @default.
• W2189607413 hasConcept C111368507 @default.
• W2189607413 hasConcept C121332964 @default.
• W2189607413 hasConcept C127313418 @default.
• W2189607413 hasConcept C132651083 @default.
• W2189607413 hasConcept C140345934 @default.
• W2189607413 hasConcept C166957645 @default.
• W2189607413 hasConcept C171878925 @default.
• W2189607413 hasConcept C191897082 @default.
• W2189607413 hasConcept C192562407 @default.
• W2189607413 hasConcept C205649164 @default.
• W2189607413 hasConcept C24890656 @default.
• W2189607413 hasConcept C2776638177 @default.
• W2189607413 hasConcept C2778883040 @default.
• W2189607413 hasConcept C2781291010 @default.
• W2189607413 hasConcept C4646841 @default.
• W2189607413 hasConcept C526406351 @default.
• W2189607413 hasConcept C53570757 @default.
• W2189607413 hasConceptScore W2189607413C100970517 @default.
• W2189607413 hasConceptScore W2189607413C111368507 @default.
• W2189607413 hasConceptScore W2189607413C121332964 @default.
• W2189607413 hasConceptScore W2189607413C127313418 @default.
• W2189607413 hasConceptScore W2189607413C132651083 @default.

• next