FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3036834242> ?p ?o ?g. }

• W3036834242 endingPage "107295" @default.
• W3036834242 startingPage "107295" @default.
• W3036834242 abstract "We demonstrate the utility of a multi-pronged approach to geomorphological studies. We show how the synthesis of results from 3-D imaging, varied geotechnical methods, and dating, reveals hitherto unknown features of a cave and of its sediment infill, and elucidates its geomorphological history. The Unicorn Cave (Einhornhöhle, southern Harz Mountains, Germany), long famous for its cave bear, lion, and mammoth fossils, is a dry vadose trunk cave high above base level, characterized by large rooms connected by shallow passages, and filled with sediments up to 40 m thick. The sediment is an archive for natural and anthropogenic environmental change: the succession of river gravels, breccia, and silts and sands provides a paleo-geomorphic and climatic archive; while human artefacts from the Paleolithic period provide information about early settlement phases. Here we derive a detailed description of the Unicorn Cave and its sediment infill by utilising several sources: (i) We synthesise data from the literature into a comprehensive picture of the sediment infill; (ii) We present new geophysical measurements of the sediments in the large room Leibnizhalle, and discuss these new measurements in view of our older findings; (iii) We map the larger chambers with the photogrammetric structure-from-motion method to build three-dimensional models; (iv) We present new age estimates from speleothem samples in the cave and discuss them with other, published, age estimates. Finally we use our newly collected evidence to reconstruct the evolution of the entire Unicorn Cave (including the newly-revealed, not-yet-accessible passages and their pristine sediment infill, as yet undisturbed by fossil hunters). The main period of speleogenesis ended with base-level incision in the mid-Pleistocene; the deposition of basal river gravels, probably in the late Cromerian, was followed by a sequence of clays and loams, capped by speleothem at ~MIS 3; the dates suggest at least two bone beds (MIS 3, and MIS 5e), along with bone material older than MIS 7." @default.
• W3036834242 created "2020-06-25" @default.
• W3036834242 creator A5015766123 @default.
• W3036834242 creator A5028919354 @default.
• W3036834242 creator A5045859506 @default.
• W3036834242 creator A5048170992 @default.
• W3036834242 date "2020-10-01" @default.
• W3036834242 modified "2023-09-25" @default.
• W3036834242 title "The sediment record of the Unicorn Cave, southern Harz Mountains, Germany" @default.
• W3036834242 cites W2008875043 @default.
• W3036834242 cites W2018314772 @default.
• W3036834242 cites W2023899869 @default.
• W3036834242 cites W2025460335 @default.
• W3036834242 cites W2027254180 @default.
• W3036834242 cites W2035822908 @default.
• W3036834242 cites W2039099009 @default.
• W3036834242 cites W2061126774 @default.
• W3036834242 cites W2077208327 @default.
• W3036834242 cites W2157663126 @default.
• W3036834242 cites W2794733902 @default.
• W3036834242 cites W2889444809 @default.
• W3036834242 cites W4249751050 @default.
• W3036834242 doi "https://doi.org/10.1016/j.geomorph.2020.107295" @default.
• W3036834242 hasPublicationYear "2020" @default.
• W3036834242 type Work @default.
• W3036834242 sameAs 3036834242 @default.
• W3036834242 citedByCount "1" @default.
• W3036834242 countsByYear W30368342422023 @default.
• W3036834242 crossrefType "journal-article" @default.
• W3036834242 hasAuthorship W3036834242A5015766123 @default.
• W3036834242 hasAuthorship W3036834242A5028919354 @default.
• W3036834242 hasAuthorship W3036834242A5045859506 @default.
• W3036834242 hasAuthorship W3036834242A5048170992 @default.
• W3036834242 hasConcept C114793014 @default.
• W3036834242 hasConcept C127313418 @default.
• W3036834242 hasConcept C151730666 @default.
• W3036834242 hasConcept C166957645 @default.
• W3036834242 hasConcept C171878925 @default.
• W3036834242 hasConcept C205649164 @default.
• W3036834242 hasConcept C2778883040 @default.
• W3036834242 hasConcept C2780734062 @default.
• W3036834242 hasConcept C2816523 @default.
• W3036834242 hasConceptScore W3036834242C114793014 @default.
• W3036834242 hasConceptScore W3036834242C127313418 @default.
• W3036834242 hasConceptScore W3036834242C151730666 @default.
• W3036834242 hasConceptScore W3036834242C166957645 @default.
• W3036834242 hasConceptScore W3036834242C171878925 @default.
• W3036834242 hasConceptScore W3036834242C205649164 @default.
• W3036834242 hasConceptScore W3036834242C2778883040 @default.
• W3036834242 hasConceptScore W3036834242C2780734062 @default.
• W3036834242 hasConceptScore W3036834242C2816523 @default.
• W3036834242 hasFunder F4320320879 @default.
• W3036834242 hasLocation W30368342421 @default.
• W3036834242 hasOpenAccess W3036834242 @default.
• W3036834242 hasPrimaryLocation W30368342421 @default.
• W3036834242 hasRelatedWork W2059791812 @default.
• W3036834242 hasRelatedWork W2076746046 @default.
• W3036834242 hasRelatedWork W2114543022 @default.
• W3036834242 hasRelatedWork W2139404099 @default.
• W3036834242 hasRelatedWork W2290802763 @default.
• W3036834242 hasRelatedWork W2328574951 @default.
• W3036834242 hasRelatedWork W2484350614 @default.
• W3036834242 hasRelatedWork W2808026184 @default.
• W3036834242 hasRelatedWork W2898342437 @default.
• W3036834242 hasRelatedWork W3209710855 @default.
• W3036834242 hasVolume "367" @default.
• W3036834242 isParatext "false" @default.
• W3036834242 isRetracted "false" @default.
• W3036834242 magId "3036834242" @default.
• W3036834242 workType "article" @default.