FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4385955922> ?p ?o ?g. }

• W4385955922 endingPage "501" @default.
• W4385955922 startingPage "490" @default.
• W4385955922 abstract "The complex Geological Conservation Review (GCR) site at Clacton-on-Sea, Essex, was notified in 1986 as a Site of Special Scientific Interest. It is an internationally important geosite and Britain's only Lower Palaeolithic type locality, giving its name to the Clactonian stone-tool industry. Fossil- and artefact-bearing channel-fill deposits laid down by the River Thames ~ 420,000 years ago, during the Hoxnian Interglacial (Marine Isotope Stage 11c), have been observed in foreshore and cliff exposures, and beneath developed and open ground in an inland arcuate footprint. These sediments provide a record of the lower reaches and estuary of the Thames during this lengthy and warm interglacial, an important partial analogue for the Holocene. Palaeoclimatic and palaeoecological evidence has been obtained from assemblages of fossil molluscs, ostracods and vertebrates, together with pollen and plant macrofossils; Clacton is also the type locality for several of the represented animal taxa, including the biostratigraphically significant ostracod Scottia browniana and a large subspecies of fallow deer, Dama dama clactoniana. This paper provides an overview of the continuing importance of the Clacton GCR site and Site of Special Scientific Interest (SSSI), summarizing recently acquired data that have enhanced understanding of the Hoxnian and the palaeoenvironments that prevailed at the time of deposition. The wider geosite has benefitted from sustained Palaeolithic archaeological interest, with the local planning authority mandating investigation of the sediments as a condition for development projects. SSSI status ensures that the significant collections of palaeontological and archaeological material amassed from the Clacton deposits over almost two centuries can be related to their context, and studies of both these archived collections and new material from the protected in situ sediments continue to provide new data and contribute to the development of cutting-edge techniques." @default.
• W4385955922 created "2023-08-18" @default.
• W4385955922 creator A5010422488 @default.
• W4385955922 creator A5024127422 @default.
• W4385955922 creator A5028413723 @default.
• W4385955922 creator A5085090223 @default.
• W4385955922 date "2023-08-01" @default.
• W4385955922 modified "2023-10-17" @default.
• W4385955922 title "The Clacton-on-Sea (Essex, UK) GCR site and SSSI: New data and continuing importance" @default.
• W4385955922 cites W10716146 @default.
• W4385955922 cites W1510205894 @default.
• W4385955922 cites W1586403601 @default.
• W4385955922 cites W1966893870 @default.
• W4385955922 cites W1966936002 @default.
• W4385955922 cites W1968071871 @default.
• W4385955922 cites W1968300582 @default.
• W4385955922 cites W1971821926 @default.
• W4385955922 cites W1973944649 @default.
• W4385955922 cites W1975766217 @default.
• W4385955922 cites W1979029804 @default.
• W4385955922 cites W1982447804 @default.
• W4385955922 cites W2001669950 @default.
• W4385955922 cites W2005477610 @default.
• W4385955922 cites W2006141262 @default.
• W4385955922 cites W2009172789 @default.
• W4385955922 cites W2014238392 @default.
• W4385955922 cites W2017191372 @default.
• W4385955922 cites W2017895953 @default.
• W4385955922 cites W2024381169 @default.
• W4385955922 cites W2025710852 @default.
• W4385955922 cites W2032074967 @default.
• W4385955922 cites W2034110281 @default.
• W4385955922 cites W2036957974 @default.
• W4385955922 cites W2039407420 @default.
• W4385955922 cites W2040391948 @default.
• W4385955922 cites W2044509513 @default.
• W4385955922 cites W2053552506 @default.
• W4385955922 cites W2064725043 @default.
• W4385955922 cites W2066187850 @default.
• W4385955922 cites W2074855159 @default.
• W4385955922 cites W2076537463 @default.
• W4385955922 cites W2077366241 @default.
• W4385955922 cites W2083430659 @default.
• W4385955922 cites W2085039530 @default.
• W4385955922 cites W2088513909 @default.
• W4385955922 cites W2102070243 @default.
• W4385955922 cites W2104155667 @default.
• W4385955922 cites W2113425021 @default.
• W4385955922 cites W2120570777 @default.
• W4385955922 cites W2135604858 @default.
• W4385955922 cites W2137455962 @default.
• W4385955922 cites W2139052267 @default.
• W4385955922 cites W2150561388 @default.
• W4385955922 cites W2155258418 @default.
• W4385955922 cites W2162050747 @default.
• W4385955922 cites W2162808698 @default.
• W4385955922 cites W2165434218 @default.
• W4385955922 cites W2167204540 @default.
• W4385955922 cites W2186180080 @default.
• W4385955922 cites W2258755779 @default.
• W4385955922 cites W2313448159 @default.
• W4385955922 cites W2325617010 @default.
• W4385955922 cites W2329685512 @default.
• W4385955922 cites W2474996639 @default.
• W4385955922 cites W2762320511 @default.
• W4385955922 cites W3017041798 @default.
• W4385955922 cites W3107120896 @default.
• W4385955922 cites W3151155246 @default.
• W4385955922 cites W3185479670 @default.
• W4385955922 cites W3195949448 @default.
• W4385955922 cites W4296557300 @default.
• W4385955922 cites W4309402775 @default.
• W4385955922 cites W4309890418 @default.
• W4385955922 cites W4381251036 @default.
• W4385955922 doi "https://doi.org/10.1016/j.pgeola.2023.07.007" @default.
• W4385955922 hasPublicationYear "2023" @default.
• W4385955922 type Work @default.
• W4385955922 citedByCount "0" @default.
• W4385955922 crossrefType "journal-article" @default.
• W4385955922 hasAuthorship W4385955922A5010422488 @default.
• W4385955922 hasAuthorship W4385955922A5024127422 @default.
• W4385955922 hasAuthorship W4385955922A5028413723 @default.
• W4385955922 hasAuthorship W4385955922A5085090223 @default.
• W4385955922 hasBestOaLocation W43859559221 @default.
• W4385955922 hasConcept C127313418 @default.
• W4385955922 hasConcept C140345934 @default.
• W4385955922 hasConcept C151730666 @default.
• W4385955922 hasConcept C164139821 @default.
• W4385955922 hasConcept C166957645 @default.
• W4385955922 hasConcept C186240526 @default.
• W4385955922 hasConcept C18903297 @default.
• W4385955922 hasConcept C205649164 @default.
• W4385955922 hasConcept C25868968 @default.
• W4385955922 hasConcept C2776608160 @default.
• W4385955922 hasConcept C2777461261 @default.
• W4385955922 hasConcept C53570757 @default.
• W4385955922 hasConcept C58642233 @default.
• W4385955922 hasConcept C71640776 @default.

• next