Matches in SemOpenAlex for { <https://semopenalex.org/work/W2014208081> ?p ?o ?g. }
Showing items 1 to 97 of
97
with 100 items per page.
- W2014208081 endingPage "2228" @default.
- W2014208081 startingPage "2219" @default.
- W2014208081 abstract "Lakes Samra, Lisan and the Dead Sea occupied the Dead Sea basin during the Last Interglacial (∼140–75 ka BP), last glacial (∼70–14 ka BP) and Holocene periods, respectively. The age of Lake Lisan and Samra was determined by U–Th dating of primary aragonites comprising parts of the lacustrine sedimentary sequences. The lakes have periodically deposited sequences of layered calcitic marls (Lake Samra) or laminated primary aragonite (Lake Lisan). The deposition of aragonite as the primary carbonate phase reflects the contribution of the incoming freshwater (loaded with bi-carbonate) and high Mg-, Ca-chloride brine that originated from the subsurface vicinity of the Dead Sea basin. Deposition of calcitic marls suggests a minor effect of the brines. The Ca-chloride subsurface brine has been migrating in and out of the wall rocks of the Dead Sea basin, reflecting the regional hydrological conditions. During most of the last glacial period and during the late Holocene, sufficient precipitation above the Judea Mountains pushed the subsurface Ca-chloride brines into the lakes causing the deposition of aragonite. During the Last Interglacial period the rain that precipitated above the Judea Mountains was insufficient to induce brine flow toward Lake Samra. It appears that sporadic floods provided calcium, bicarbonate and detritus to produce the Samra calcitic marls. Travertines deposited at the Samra–Lisan boundary indicate the early stage in the resumption of groundwater (springs) activity that led to the resurgence of Ca-chloride brine and rise of Lake Lisan. Similar variations in the regional rain precipitation and hydrological activity probably characterized the long-term geochemical evolution of Pleistocene lacustrine water-bodies in the Dead Sea basin, enabling the use of the carbonates as paleo-hydrological monitors." @default.
- W2014208081 created "2016-06-24" @default.
- W2014208081 creator A5047711922 @default.
- W2014208081 creator A5063727388 @default.
- W2014208081 creator A5078612470 @default.
- W2014208081 date "2007-09-01" @default.
- W2014208081 modified "2023-10-16" @default.
- W2014208081 title "Primary carbonates and Ca-chloride brines as monitors of a paleo-hydrological regime in the Dead Sea basin" @default.
- W2014208081 cites W1984512200 @default.
- W2014208081 cites W1994100779 @default.
- W2014208081 cites W1997116381 @default.
- W2014208081 cites W2006914133 @default.
- W2014208081 cites W2011008320 @default.
- W2014208081 cites W2038464013 @default.
- W2014208081 cites W2040060926 @default.
- W2014208081 cites W2046373624 @default.
- W2014208081 cites W2047116097 @default.
- W2014208081 cites W2064781474 @default.
- W2014208081 cites W2072416217 @default.
- W2014208081 cites W2079151177 @default.
- W2014208081 cites W2087901843 @default.
- W2014208081 cites W2095648000 @default.
- W2014208081 cites W2128123878 @default.
- W2014208081 cites W2151689777 @default.
- W2014208081 cites W2165741265 @default.
- W2014208081 cites W2460937285 @default.
- W2014208081 cites W299954433 @default.
- W2014208081 doi "https://doi.org/10.1016/j.quascirev.2007.04.019" @default.
- W2014208081 hasPublicationYear "2007" @default.
- W2014208081 type Work @default.
- W2014208081 sameAs 2014208081 @default.
- W2014208081 citedByCount "47" @default.
- W2014208081 countsByYear W20142080812012 @default.
- W2014208081 countsByYear W20142080812013 @default.
- W2014208081 countsByYear W20142080812014 @default.
- W2014208081 countsByYear W20142080812015 @default.
- W2014208081 countsByYear W20142080812016 @default.
- W2014208081 countsByYear W20142080812017 @default.
- W2014208081 countsByYear W20142080812018 @default.
- W2014208081 countsByYear W20142080812019 @default.
- W2014208081 countsByYear W20142080812020 @default.
- W2014208081 countsByYear W20142080812021 @default.
- W2014208081 crossrefType "journal-article" @default.
- W2014208081 hasAuthorship W2014208081A5047711922 @default.
- W2014208081 hasAuthorship W2014208081A5063727388 @default.
- W2014208081 hasAuthorship W2014208081A5078612470 @default.
- W2014208081 hasConcept C109007969 @default.
- W2014208081 hasConcept C111368507 @default.
- W2014208081 hasConcept C114793014 @default.
- W2014208081 hasConcept C127313418 @default.
- W2014208081 hasConcept C140345934 @default.
- W2014208081 hasConcept C15739521 @default.
- W2014208081 hasConcept C17409809 @default.
- W2014208081 hasConcept C186240526 @default.
- W2014208081 hasConcept C191897082 @default.
- W2014208081 hasConcept C192562407 @default.
- W2014208081 hasConcept C2779866092 @default.
- W2014208081 hasConcept C2780191791 @default.
- W2014208081 hasConcept C2780659211 @default.
- W2014208081 hasConcept C6494504 @default.
- W2014208081 hasConcept C92927620 @default.
- W2014208081 hasConceptScore W2014208081C109007969 @default.
- W2014208081 hasConceptScore W2014208081C111368507 @default.
- W2014208081 hasConceptScore W2014208081C114793014 @default.
- W2014208081 hasConceptScore W2014208081C127313418 @default.
- W2014208081 hasConceptScore W2014208081C140345934 @default.
- W2014208081 hasConceptScore W2014208081C15739521 @default.
- W2014208081 hasConceptScore W2014208081C17409809 @default.
- W2014208081 hasConceptScore W2014208081C186240526 @default.
- W2014208081 hasConceptScore W2014208081C191897082 @default.
- W2014208081 hasConceptScore W2014208081C192562407 @default.
- W2014208081 hasConceptScore W2014208081C2779866092 @default.
- W2014208081 hasConceptScore W2014208081C2780191791 @default.
- W2014208081 hasConceptScore W2014208081C2780659211 @default.
- W2014208081 hasConceptScore W2014208081C6494504 @default.
- W2014208081 hasConceptScore W2014208081C92927620 @default.
- W2014208081 hasIssue "17-18" @default.
- W2014208081 hasLocation W20142080811 @default.
- W2014208081 hasOpenAccess W2014208081 @default.
- W2014208081 hasPrimaryLocation W20142080811 @default.
- W2014208081 hasRelatedWork W1984444890 @default.
- W2014208081 hasRelatedWork W2010292714 @default.
- W2014208081 hasRelatedWork W2056627274 @default.
- W2014208081 hasRelatedWork W2142942236 @default.
- W2014208081 hasRelatedWork W2156725572 @default.
- W2014208081 hasRelatedWork W2252314226 @default.
- W2014208081 hasRelatedWork W2517646385 @default.
- W2014208081 hasRelatedWork W3097437618 @default.
- W2014208081 hasRelatedWork W3111083456 @default.
- W2014208081 hasRelatedWork W3147553687 @default.
- W2014208081 hasVolume "26" @default.
- W2014208081 isParatext "false" @default.
- W2014208081 isRetracted "false" @default.
- W2014208081 magId "2014208081" @default.
- W2014208081 workType "article" @default.