FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2064755562> ?p ?o ?g. }

• W2064755562 endingPage "214" @default.
• W2064755562 startingPage "206" @default.
• W2064755562 abstract "This paper focuses on the reconstruction of Holocene climatic and environmental changes in two archaeological sites of southwestern and north-central Calabria (southern Italy). It is based on a comparison of geoarchaeological, pedological and pedoanthracological data from soil profiles in the coastal hilly and inland mountainous surroundings of Palmi and Cecita Lake, respectively. At the Palmi site, the representative soil profile includes settlements and artefacts ranging from late Neolithic to late early Bronze Age and undifferentiated historical epochs. The archaeological record of soils at Cecita spans from late Neolithic/early Eneolithic to Roman ages. At both sites, surface A horizons are affected by repeated plough marks. All soils display some Andisol-like features, related to some volcanic input during soil formation originating from late Pleistocene to Holocene explosive eruptions of the Aeolian Islands. The occurrence of clay coatings, their relict nature and overall dominant phyllosilicate clay minerals in the Neolithic soil horizons of both sites, suggest warm climate conditions with high moisture availability and some seasonal contrast, during the late early-middle Holocene climatic optimum. The post-Neolithic soils show comparable or more abundant amounts of short-range order minerals than phyllosilicates, and no to scarce clay coatings. These features indicate a transition towards (probably cooler) prolonged humid conditions, intercalated by one or more drought episodes. Severe land degradation is recorded between these major climatic phases, indicated by human impact (deforestation and agriculture) and soil erosion. Soil charcoal analysis from Cecita soils provide evidence of these anthropogenic environmental changes, as indicated by the dominance of deciduous oak forest in Neolithic soils, followed by a transition to a mountain pine forest recorded in the Roman soils. A deciduous oak forest characterizes the vegetation at Palmi from the Neolithic onward." @default.
• W2064755562 created "2016-06-24" @default.
• W2064755562 creator A5006300504 @default.
• W2064755562 creator A5019190552 @default.
• W2064755562 creator A5026488280 @default.
• W2064755562 creator A5050063983 @default.
• W2064755562 creator A5059361259 @default.
• W2064755562 creator A5061464029 @default.
• W2064755562 creator A5064347556 @default.
• W2064755562 creator A5067227595 @default.
• W2064755562 creator A5077128025 @default.
• W2064755562 date "2013-03-01" @default.
• W2064755562 modified "2023-10-16" @default.
• W2064755562 title "Reconstruction of Holocene environmental changes in two archaeological sites of Calabria (Southern Italy) using an integrated pedological and anthracological approach" @default.
• W2064755562 cites W1510488104 @default.
• W2064755562 cites W1528536974 @default.
• W2064755562 cites W1990972185 @default.
• W2064755562 cites W1996052557 @default.
• W2064755562 cites W1998193050 @default.
• W2064755562 cites W2009931761 @default.
• W2064755562 cites W2010756342 @default.
• W2064755562 cites W2010889515 @default.
• W2064755562 cites W2017141417 @default.
• W2064755562 cites W2028643338 @default.
• W2064755562 cites W2029742834 @default.
• W2064755562 cites W2032621606 @default.
• W2064755562 cites W2039926974 @default.
• W2064755562 cites W2042904173 @default.
• W2064755562 cites W2043842533 @default.
• W2064755562 cites W2050283325 @default.
• W2064755562 cites W2052005956 @default.
• W2064755562 cites W2053566298 @default.
• W2064755562 cites W2055106657 @default.
• W2064755562 cites W2063217350 @default.
• W2064755562 cites W2070010015 @default.
• W2064755562 cites W2076814911 @default.
• W2064755562 cites W2082403376 @default.
• W2064755562 cites W2085002143 @default.
• W2064755562 cites W2085094021 @default.
• W2064755562 cites W2087309847 @default.
• W2064755562 cites W2088712252 @default.
• W2064755562 cites W2089025642 @default.
• W2064755562 cites W2089057218 @default.
• W2064755562 cites W2093367842 @default.
• W2064755562 cites W2112291891 @default.
• W2064755562 cites W2120637384 @default.
• W2064755562 cites W2131945198 @default.
• W2064755562 cites W2136246993 @default.
• W2064755562 cites W2145253618 @default.
• W2064755562 cites W2151794823 @default.
• W2064755562 cites W2160579273 @default.
• W2064755562 cites W222588158 @default.
• W2064755562 cites W4231878032 @default.
• W2064755562 doi "https://doi.org/10.1016/j.quaint.2011.12.006" @default.
• W2064755562 hasPublicationYear "2013" @default.
• W2064755562 type Work @default.
• W2064755562 sameAs 2064755562 @default.
• W2064755562 citedByCount "15" @default.
• W2064755562 countsByYear W20647555622013 @default.
• W2064755562 countsByYear W20647555622014 @default.
• W2064755562 countsByYear W20647555622015 @default.
• W2064755562 countsByYear W20647555622016 @default.
• W2064755562 countsByYear W20647555622017 @default.
• W2064755562 countsByYear W20647555622023 @default.
• W2064755562 crossrefType "journal-article" @default.
• W2064755562 hasAuthorship W2064755562A5006300504 @default.
• W2064755562 hasAuthorship W2064755562A5019190552 @default.
• W2064755562 hasAuthorship W2064755562A5026488280 @default.
• W2064755562 hasAuthorship W2064755562A5050063983 @default.
• W2064755562 hasAuthorship W2064755562A5059361259 @default.
• W2064755562 hasAuthorship W2064755562A5061464029 @default.
• W2064755562 hasAuthorship W2064755562A5064347556 @default.
• W2064755562 hasAuthorship W2064755562A5067227595 @default.
• W2064755562 hasAuthorship W2064755562A5077128025 @default.
• W2064755562 hasConcept C127313418 @default.
• W2064755562 hasConcept C140345934 @default.
• W2064755562 hasConcept C166957645 @default.
• W2064755562 hasConcept C205649164 @default.
• W2064755562 hasConceptScore W2064755562C127313418 @default.
• W2064755562 hasConceptScore W2064755562C140345934 @default.
• W2064755562 hasConceptScore W2064755562C166957645 @default.
• W2064755562 hasConceptScore W2064755562C205649164 @default.
• W2064755562 hasLocation W20647555621 @default.
• W2064755562 hasOpenAccess W2064755562 @default.
• W2064755562 hasPrimaryLocation W20647555621 @default.
• W2064755562 hasRelatedWork W2023221316 @default.
• W2064755562 hasRelatedWork W2049853283 @default.
• W2064755562 hasRelatedWork W2391280628 @default.
• W2064755562 hasRelatedWork W2748952813 @default.
• W2064755562 hasRelatedWork W2899084033 @default.
• W2064755562 hasRelatedWork W3141051090 @default.
• W2064755562 hasRelatedWork W3142304672 @default.
• W2064755562 hasRelatedWork W3146394291 @default.
• W2064755562 hasRelatedWork W4294323257 @default.
• W2064755562 hasRelatedWork W862072336 @default.
• W2064755562 hasVolume "288" @default.
• W2064755562 isParatext "false" @default.
• W2064755562 isRetracted "false" @default.

• next