FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4309609563> ?p ?o ?g. }

• W4309609563 abstract "Deep-sea anoxic brine pools are unique and extreme, yet habitable environments. However, their extent and processes of formation are not fully understood. Using geophysical analysis and seafloor surveying, we discovered the eastmost brine pools known in the ultraoligotrophic Eastern Mediterranean Sea, at the Palmahim Disturbance offshore Israel (~1150 m water depth). These brine pools are located directly above a ~1km wide piece of the Messinian evaporites section, which was up thrusted to ~350 m below the seafloor. We sampled brines and short cores to characterize the chemical composition of several small (up to 5m diameter) anoxic, methanic and warm (21.6°C) brine pools and adjacent seafloor sediments porewater. The maximal salinities measured at the pools and adjacent porewater were 63.9 and 72 PSU, respectively. The brines are characterized by enriched Na and Cl concentrations by a factor of ~1.8 and depleted Mg, SO 4 , K and Ca contents by factors of circa 6, 3, 2 and ~1.3, respectively, compared to the ambient seawater. Relations of the major element concentrations reveal a mixing curve between seawater and enriched Na/Cl and depleted Mg/Cl, K/Cl and SO 4 /Cl end-members, and do not coincide with relics of fossil residual evaporated seawater. We propose their composition reflects: 1) dissolution of Messinian halite (NaCl) by seawater, supported by their low Br/Cl ratios; 2) additional small rise in Na/Cl ratios due to the impact of clay mineral dehydration or/and dissolution of trace (~1% of the Na) amounts of detrital trona (Na 3 H(CO 3 ) 2 •2H 2 0), coinciding with the enriched alkalinity concentrations; 3) diagenesis processes depleting Mg, K and SO 4 , mainly by the formation of authigenic K-rich Mg-smectite, clay mineral dehydration, dolomitization/Mg-calcite precipitation and redox processes. The δ 18 O and δD values of the Palmahim brine may reflect the impact of clay mineral dehydration. Comparison to all other East Mediterranean brine lakes shows that the Palmahim brine pool system represents similar provenance of brines as observed for the Eastern Mediterranean Napoli, Nadir and Tyro lakes, while potentially recording additional processes attributed to its proximity to the coastal area." @default.
• W4309609563 created "2022-11-28" @default.
• W4309609563 creator A5009947929 @default.
• W4309609563 creator A5030098778 @default.
• W4309609563 creator A5035419856 @default.
• W4309609563 creator A5037241072 @default.
• W4309609563 creator A5061936043 @default.
• W4309609563 creator A5063999000 @default.
• W4309609563 creator A5066306567 @default.
• W4309609563 creator A5073871824 @default.
• W4309609563 creator A5085396512 @default.
• W4309609563 creator A5088996823 @default.
• W4309609563 creator A5091334646 @default.
• W4309609563 date "2022-11-17" @default.
• W4309609563 modified "2023-10-13" @default.
• W4309609563 title "Discovery and chemical composition of the eastmost deep-sea anoxic brine pools in the Eastern Mediterranean Sea" @default.
• W4309609563 cites W1635838947 @default.
• W4309609563 cites W1878921959 @default.
• W4309609563 cites W1901073443 @default.
• W4309609563 cites W1931611046 @default.
• W4309609563 cites W1969006113 @default.
• W4309609563 cites W1969692530 @default.
• W4309609563 cites W1976690501 @default.
• W4309609563 cites W1977298149 @default.
• W4309609563 cites W1983910781 @default.
• W4309609563 cites W1984304540 @default.
• W4309609563 cites W1991468612 @default.
• W4309609563 cites W2010714875 @default.
• W4309609563 cites W2017500079 @default.
• W4309609563 cites W2018228272 @default.
• W4309609563 cites W2024961541 @default.
• W4309609563 cites W2025296492 @default.
• W4309609563 cites W2026948106 @default.
• W4309609563 cites W2027206314 @default.
• W4309609563 cites W2029075053 @default.
• W4309609563 cites W2032996695 @default.
• W4309609563 cites W2039248536 @default.
• W4309609563 cites W2039783600 @default.
• W4309609563 cites W2040558728 @default.
• W4309609563 cites W2040964459 @default.
• W4309609563 cites W2044666219 @default.
• W4309609563 cites W2046553642 @default.
• W4309609563 cites W2047286747 @default.
• W4309609563 cites W2048100073 @default.
• W4309609563 cites W2050664154 @default.
• W4309609563 cites W2056561483 @default.
• W4309609563 cites W2060177855 @default.
• W4309609563 cites W2067910389 @default.
• W4309609563 cites W2081162017 @default.
• W4309609563 cites W2098307955 @default.
• W4309609563 cites W2108120392 @default.
• W4309609563 cites W2112019984 @default.
• W4309609563 cites W2117588612 @default.
• W4309609563 cites W2118215057 @default.
• W4309609563 cites W2132638924 @default.
• W4309609563 cites W2134712896 @default.
• W4309609563 cites W2141698562 @default.
• W4309609563 cites W2162559981 @default.
• W4309609563 cites W2166304646 @default.
• W4309609563 cites W2288181389 @default.
• W4309609563 cites W2610379404 @default.
• W4309609563 cites W2742222607 @default.
• W4309609563 cites W2748359477 @default.
• W4309609563 cites W2788072225 @default.
• W4309609563 cites W2802474352 @default.
• W4309609563 cites W2804217194 @default.
• W4309609563 cites W2808486042 @default.
• W4309609563 cites W2891337572 @default.
• W4309609563 cites W2913184755 @default.
• W4309609563 cites W2941836810 @default.
• W4309609563 cites W2944141856 @default.
• W4309609563 cites W2979023586 @default.
• W4309609563 cites W2999375046 @default.
• W4309609563 cites W3106896859 @default.
• W4309609563 cites W3113443506 @default.
• W4309609563 cites W3125301578 @default.
• W4309609563 cites W3205534211 @default.
• W4309609563 cites W4283593850 @default.
• W4309609563 cites W4293085093 @default.
• W4309609563 cites W653957838 @default.
• W4309609563 doi "https://doi.org/10.3389/fmars.2022.1040681" @default.
• W4309609563 hasPublicationYear "2022" @default.
• W4309609563 type Work @default.
• W4309609563 citedByCount "6" @default.
• W4309609563 countsByYear W43096095632023 @default.
• W4309609563 crossrefType "journal-article" @default.
• W4309609563 hasAuthorship W4309609563A5009947929 @default.
• W4309609563 hasAuthorship W4309609563A5030098778 @default.
• W4309609563 hasAuthorship W4309609563A5035419856 @default.
• W4309609563 hasAuthorship W4309609563A5037241072 @default.
• W4309609563 hasAuthorship W4309609563A5061936043 @default.
• W4309609563 hasAuthorship W4309609563A5063999000 @default.
• W4309609563 hasAuthorship W4309609563A5066306567 @default.
• W4309609563 hasAuthorship W4309609563A5073871824 @default.
• W4309609563 hasAuthorship W4309609563A5085396512 @default.
• W4309609563 hasAuthorship W4309609563A5088996823 @default.
• W4309609563 hasAuthorship W4309609563A5091334646 @default.
• W4309609563 hasBestOaLocation W43096095631 @default.
• W4309609563 hasConcept C107872376 @default.
• W4309609563 hasConcept C108970007 @default.

• next