FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4256486871> ?p ?o ?g. }

• W4256486871 abstract "The two large lakes named Samra and Lisan existed in the Dead Sea graben from 350,000 to 120,000B.p. and 60,000 to 12,000B.p. Their sediments tentatively are correlated with the European Riss and Würm glacial epochs. Thick marls are the chief sediments in the deep water north basin. Rocksalt deposition dominated within the troughs of both north and south basins throughout the intervening Riss-Würm Interglacial stage. Lithology of Lisan Formation (Würm) in that basin indicates rapid and extreme fluctuations of level. Eight major climatic cycles are recorded during Würm glaciation when the level fluctuated between -180 m m.s.l. and probably lower than -400 m m.s.l. Rocksalt was deposited within both basins during warm dry phases of the Lisan stage. At the present state of knowledge no specific tectonic or volcanic activities can be tied to these climatic events. The Holocene Period was similar lithologically to that of the Lisan Formation and transition between them was gradual. Primarily the difference between the two was change in relative time span between alternate wet and dry phases. Dry phases of Holocene gradually became longer while wet ones with Dead Sea transgressions became shorter. Tectonic regimes during the first part—the Natufian age to Early Bronze III, 12,000 to 4400 B.P.—seem to have been milder than later ones, end of Early Bronze III to the present. The severe earthquake that destroyed Sodom and Gomorrah in 4350 B.P. was followed by a 300-year long subphase of gradually warming climate that became extremely dry during the latter part of the Intermediate Bronze age. Climatic Wet Phase III began about 3900 B.P. It was the longest, about 800 years, and most intense wet phase of Holocene and it probably was associated with volcanism. No abrupt cultural or demographic changes are known during transition from Epi-Paleolithic or Geometric Kebaran from the last glacial phase of the Pleistocene Period through Natufian to the early part of Holocene Pre-Pottery Neolithic. The reason for this stability is not clear especially because average temperatures of global oceans during the latest Pleistocene glaciation were appreciably lower than those during Early Holocene (Emiliani, 1978)." @default.
• W4256486871 created "2022-05-12" @default.
• W4256486871 creator A5014064936 @default.
• W4256486871 creator A5057629510 @default.
• W4256486871 date "1995-11-09" @default.
• W4256486871 modified "2023-09-23" @default.
• W4256486871 title "Synopsis" @default.
• W4256486871 doi "https://doi.org/10.1093/oso/9780195090949.003.0010" @default.
• W4256486871 hasPublicationYear "1995" @default.
• W4256486871 type Work @default.
• W4256486871 citedByCount "0" @default.
• W4256486871 crossrefType "book-chapter" @default.
• W4256486871 hasAuthorship W4256486871A5014064936 @default.
• W4256486871 hasAuthorship W4256486871A5057629510 @default.
• W4256486871 hasConcept C100970517 @default.
• W4256486871 hasConcept C109007969 @default.
• W4256486871 hasConcept C114793014 @default.
• W4256486871 hasConcept C121332964 @default.
• W4256486871 hasConcept C122792734 @default.
• W4256486871 hasConcept C127313418 @default.
• W4256486871 hasConcept C140345934 @default.
• W4256486871 hasConcept C151730666 @default.
• W4256486871 hasConcept C15739521 @default.
• W4256486871 hasConcept C160464908 @default.
• W4256486871 hasConcept C166839181 @default.
• W4256486871 hasConcept C186240526 @default.
• W4256486871 hasConcept C205649164 @default.
• W4256486871 hasConcept C24890656 @default.
• W4256486871 hasConcept C26099304 @default.
• W4256486871 hasConcept C2776200160 @default.
• W4256486871 hasConcept C2781291010 @default.
• W4256486871 hasConcept C92927620 @default.
• W4256486871 hasConceptScore W4256486871C100970517 @default.
• W4256486871 hasConceptScore W4256486871C109007969 @default.
• W4256486871 hasConceptScore W4256486871C114793014 @default.
• W4256486871 hasConceptScore W4256486871C121332964 @default.
• W4256486871 hasConceptScore W4256486871C122792734 @default.
• W4256486871 hasConceptScore W4256486871C127313418 @default.
• W4256486871 hasConceptScore W4256486871C140345934 @default.
• W4256486871 hasConceptScore W4256486871C151730666 @default.
• W4256486871 hasConceptScore W4256486871C15739521 @default.
• W4256486871 hasConceptScore W4256486871C160464908 @default.
• W4256486871 hasConceptScore W4256486871C166839181 @default.
• W4256486871 hasConceptScore W4256486871C186240526 @default.
• W4256486871 hasConceptScore W4256486871C205649164 @default.
• W4256486871 hasConceptScore W4256486871C24890656 @default.
• W4256486871 hasConceptScore W4256486871C26099304 @default.
• W4256486871 hasConceptScore W4256486871C2776200160 @default.
• W4256486871 hasConceptScore W4256486871C2781291010 @default.
• W4256486871 hasConceptScore W4256486871C92927620 @default.
• W4256486871 hasLocation W42564868711 @default.
• W4256486871 hasOpenAccess W4256486871 @default.
• W4256486871 hasPrimaryLocation W42564868711 @default.
• W4256486871 hasRelatedWork W12524407 @default.
• W4256486871 hasRelatedWork W12580597 @default.
• W4256486871 hasRelatedWork W33467464 @default.
• W4256486871 hasRelatedWork W35018179 @default.
• W4256486871 hasRelatedWork W51517975 @default.
• W4256486871 hasRelatedWork W83169783 @default.
• W4256486871 hasRelatedWork W87031226 @default.
• W4256486871 hasRelatedWork W90405098 @default.
• W4256486871 hasRelatedWork W90577191 @default.
• W4256486871 hasRelatedWork W9200569 @default.
• W4256486871 isParatext "false" @default.
• W4256486871 isRetracted "false" @default.
• W4256486871 workType "book-chapter" @default.