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International Journal of Earth Sciences

, Volume 107, Issue 7, pp 2409–2431 | Cite as

Development of the Inland Sea and its evaporites in the Jordan-Dead Sea Transform based on hydrogeochemical considerations and the geological consequences

  • Peter Möller
  • E. Rosenthal
  • N. Inbar
  • C. Siebert
Original Paper
  • 90 Downloads

Abstract

Differences in the distribution of Na/Cl, Br/Cl and Mg/Ca equivalent values suggest a morphotectonic barrier at Marma Feiyad dividing the Tertiary Inland Sea into two basins covering the region of the Jordan Valley, Middle East. Depending on the Tethys sea level, three phases of evaporation are distinguishable that are related to three sections of the drilling log of Zemah 1. In phase 1 and 3 only the northern basin was flooded. During phase 2 both basins were inundated, but halite mainly precipitated in the southern one. The halite deposition in one or the other basin by evaporation is estimated by applying a two-box model. The results are constrained by the average subduction rate of 700–875 m/Ma and characteristic Na/Cl values of 0.52 and 0.12 in the northern and southern basin, respectively. In different scenarios the sedimentation rates of halite and non-halite components are varied due to assumed halokinesis, reshuffling of salt and erosion of non-halite sediments. These simulations suggest that periods of 450–600 and 100–170 ka in the southern and northern basin were needed, until the Na/Cl values of 0.12 and 0.52 were, respectively, attained. The Inland Sea most probably existed for 2.2 ± 0.3 Ma between 8.5 and 6.3 Ma ago (Tortonian). It was terminated at the beginning of the Messinian crisis. In all simulations the drainage flux into the southern basin exceeded that into the northern basin, suggesting that the proto-Jordan River either did not exist at that time or did not discharge into the northern basin.

Keywords

Jordan-Dead Sea Rift Valley Brine generation Halite deposition Evaporation from coupled basins Subsidence rate Period of Inland Sea 

Abbreviations

ASR

Average subsidence rate

CGC

Carbonates–gypsum–clay minerals

LSR

Apparent local subsidence rate

Re

Evaporation rate

Rp

Precipitation rate

Rhalite

Halite deposition rate

RCGC

Sedimentation rate of carbonates–gypsum–clay minerals

tapp

Time interval for approaching the steady state of selected Na/Cl values

tP

Time period of the Inland Sea

YHBS

Yizre’el–Harod–Bet She’an valley

Notes

Acknowledgements

The authors greatly acknowledge many fruitful discussions with Prof. A. Flexer, Prof. K. Bandel, Dr. Y. Greitzer, and Dr. Y. Kiro who helped by their critical comments to elucidate the geological issues in the Rift. The comments of an anonymous reviewer were gratefully accepted. This study was partially supported by the DFG project MA 4450/2.

References

  1. Anati DA, Stiller M, Shasha S, Gat JR (1987) Changes in the thermo-haline structure of the Dead Sea, 1979–1984. Earth Planet Sci Lett 84:109–121CrossRefGoogle Scholar
  2. Bandel K, Alhejoj I, Salameh E (2016) Geologic evolution of the Tertiary–Quaternary Jordan Valley with introduction of the Bakura Formation. Freib Forsch C550:103–135Google Scholar
  3. Belmaker R, Lazar B, Christl M, Tepelyakov N, Stein M (2013) 10Be dating of Neogene halite. Geochim Cosmochim Acta 122:418–429CrossRefGoogle Scholar
  4. Ben-Avraham Z (2014) Geophysical studies of the crustal structure along the Southern Dead Sea Fault. In: Garfunkel Z, Ben-Avraham Z, Kagan E (eds) Dead Sea Transform fault system: reviews, pp 1–27Google Scholar
  5. Bergelson G, Nati R, Bein A (1999) Salinisation and dilution history of groundwater discharging into the Sea of Galilee, the Dead Sea Transform, Israel. Appl Geochem 14:91–118CrossRefGoogle Scholar
  6. Buchbinder B, Zilberman E (1997) Sequence stratigraphy of Miocene–Pliocene carbonate–silicates shelf deposits in the eastern Mediterranean margin (Israel)—effects of eustasy and tectonics. Sedim Geol 112:7–32CrossRefGoogle Scholar
  7. Colacino M, Dell’Osso L (1977) Monthly mean evaporation over the Mediterranean Sea. Arch Met Geophys Bioklimat Ser A 26:283–293CrossRefGoogle Scholar
  8. Eckert W, Trüper HG (1993) Microbially-related redox changes in a subtropical lake 1. In situ monitoring of the annual redox cycle. Biogeochemistry 21:1–19CrossRefGoogle Scholar
  9. Exact (1998) Overview of the Middle East water resources. ISBN 0-607-91785-7, p 44Google Scholar
  10. Fleischer L, Gafsou R (2003) Top Judea Group—digital structural map of Israel, 1:200,000 scale, 2 sheets. The Geophysical Institute of Israel, Rep. 753/312/03Google Scholar
  11. Fleischer L, Varshavsky A (2002) A lithostratigraphic data base of oil and gas wells drilled in Israel. The Geophysical Institute of Israel, Rep. 874/202/02Google Scholar
  12. Flexer A, Yellin-Dror A (2009) Geology and tectonic setting. In: Hoetzl H, Möller P, Rosenthal E (eds) The water of the Jordan Valley. Springer, Berlin, pp 15–54CrossRefGoogle Scholar
  13. Flexer A, Yellin-Dror A, Kronfeld E, Rosenthal E, Ben Avraham Z, Artzstein PP, Davidson L (2000) A Neogene salt body as the primary source of the salinity in Lake Kinneret. Arch Hydrobiol Spec Issue Adv Limnol 55:69–85Google Scholar
  14. Frieslander U (2000) The structure of the Dead Sea Transform emphasizing the Arava using new geophysical data. Ph.D. Thesis Hebrew University of Jerusalem, p 101Google Scholar
  15. Garcia-Veigas J, Rosell L, Zak I, Playa E, Ayora C, Starinsky A (2009) Evidence of potash salt formation in the Pliocene Lagoon. Chem Geol 265:499–511CrossRefGoogle Scholar
  16. Gardosh M, Shulman H, Salhov S (1995) Findings from Amiaz East-1 and Sedom Deep-1 wells and their implications on the geology of the southern Dead Sea Basin. Isr Geol Soc Ann Meet, Zikhron Ya’aqov, p 36Google Scholar
  17. Gardosh M, Kashai E, Salhov S, Shulman H, Tannenbaum E (1997) Hydrocarbon exploration in the Dead Sea area. In: Niemi TM, Ben-Avraham Z, Gat JR (eds), The Dead Sea, pp 57–72Google Scholar
  18. Garfunkel Z (1997) The history of the formation of the Dead Sea basin. In: Niemi TM, Ben-Avraham Z, Gat JR (eds) The Dead Sea, pp 36–56Google Scholar
  19. Garfunkel Z (2014) Lateral movement and deformation along the Dead Sea Transform. In: Garfunkel Z, Ben-Avraham Z, Kagan E (eds) Dead Sea Transform fault system: reviews, pp 109–150Google Scholar
  20. Garfunkel Z, Ben-Avraham Z (2001) Basins along the Dead Sea Transform. In: Ziegler P, CavassaW, Robertson AHW, Crasqin-Soleau S (eds) Tethyan Rift/wrench basins and passive margins. Mem Museum National d’Histoire Naturelle 186, pp 607–627Google Scholar
  21. Gat JR, Mazor E, Tzur Y (1969) The stable isotope composition of mineral water in the Jordan Rift Valley. J Hydrol 16:177–211CrossRefGoogle Scholar
  22. Gvirtzman Z, Steinberg J, Buchbinder B, Zilberman E, Siman-Tov R, Calvo R, Grossovicz L (2011) Retreating Late Tertiary shorelines in Israel: implications for the exposure of north Arabia and Levant during Neotethys closure. Lithosphere 3:95–109CrossRefGoogle Scholar
  23. Herut B (1992) The chemical composition and sources of dissolved salts in rainwater in Israel. PhD-Thesis, Hebrew University of Jerusalem (in Hebrew, English Abstract)Google Scholar
  24. Hirsch F (2005) The Oligocene–Pliocene of Israel. In: Hall J, Krasheninnikov VA, Hirsch F, Benjamini C, Flexer A (eds) Geological framework of the Levant, vol II: the Levantine Basin and Israel. Art Plus, Jerusalem, pp 459–488Google Scholar
  25. Horita J, Zimmermann H, Holland HD (2002) Chemical evolution of seawater during the Phanerozoic: implications from the record of marine evaporates. Geochim Cosmochim Acta 66:3733–3756CrossRefGoogle Scholar
  26. Inbar N (2012) The evaporitic subsurface body of Kinnarot basin: Stratigraphy, Structure, Geohydrology. PhD Thesis. English. Tel Aviv University, IsraelGoogle Scholar
  27. Katz A, Starinsky A (2009) Geochemical history of the Dead Sea. Aquat Geochem 15:159–194CrossRefGoogle Scholar
  28. Kiro Y, Goldstein SL, Lazar B, Stein M (2015) Environmental implications of salt facies in the Dead Sea. GSA Bull.  https://doi.org/10.1130/B31357.1 CrossRefGoogle Scholar
  29. Klein-BenDavid O, Sass E, Katz A (2004) The evolution of marine evaporitic brines in inland basins: the Jordan-Dead Sea Rift valley. Geochim Cosmochim Acta 68:1763–1775CrossRefGoogle Scholar
  30. Knorr G, Butzin M, Micheels A, Lohmann G (2011) A warm Miocene climate at low atmospheric CO2 levels. Geophys Res Lett 39:L20701.  https://doi.org/10.1029/2011GL048873 CrossRefGoogle Scholar
  31. Magaritz M, Nadler A (1980) Re-interpretation of 18O and D isotopic composition of the Tiberias subgroup hot waters. Proc. Geol. Isr. Ann Meet Southern Sinai and the Gulf of Elat, Ophira, Sinai, Feb 1980, pp 1–26Google Scholar
  32. Marcus E, Slager J (1985) The sedimentary-magmatic sequence of the Zemah 1 well (Jordan-Dead Sea Rift, Israel) and its emplacement in time and space. Isr J Earth Sci 34:1–10Google Scholar
  33. Mazor E, Mero F (1969) Origin of the Kinneret-Noit water association in the Kinneret-Dead Sea Valley. Isr J Hydrol 7:318–333CrossRefGoogle Scholar
  34. McCaffrey MA, Lazar B, Holland HD (1987) The evaporation path of seawater and the coprecipitation of Br and K+ with halite. J Sedim Petrol 57:928–937Google Scholar
  35. Micheels A, Bruch AA, Uhl D, Utescher T, Mosbrugger V (2007) A late Miocene climate model simulation with ECHAM4/ML and its quantitative validation with terrestrial proxy data. Paleogeogr Paleoclimat Paleoecol 253:251–270CrossRefGoogle Scholar
  36. Miller KG, Kominz MA, Browning JV, Wright JD, Mountain GS, Katz ME, Sugarman PJ, Cramer BS, Christie-Blick N, Pekar SF (2005) The Phanerozoic record of global sea-level change. Sci 310:1293–1298CrossRefGoogle Scholar
  37. Mittlefehldt DW, Slager Y (1986) Petrology of the basalts and gabbros from the Zemah-1 drill hole, Jordan Rift Valley. Isr J Earth Sci 35:10–22Google Scholar
  38. Möller P, Rosenthal E, Geyer S, Guttman J (2003) Rare earths and yttrium hydrostratigraphy along the Lake Tiberias-Dead Sea-Arava transform fault, Israel and adjoining territories. Appl Geochem 18:1613–1623CrossRefGoogle Scholar
  39. Möller P, Rosenthal E, Geyer S (2009) Characterization of aquifer environments by major and minor elements and stable isotopes of sulfate. In: Hötzel H, Möller P, Rosenthal E (eds) The water of the Jordan Valley. Springer, Berlin, pp 83–121CrossRefGoogle Scholar
  40. Möller P, Siebert C, Geyer S, Inbar N, Rosenthal E, Flexer A, Zilberbrand M (2012) Relationship of brines in the Kinnarot Basin, Jordan-Dead Sea Rift Valley. Geofluids 12:166–181CrossRefGoogle Scholar
  41. Möller P, Rosenthal E, Flexer A (2014) The hydrogeochemistry of subsurface brines in and west of the Jordan-Dead Sea Transform fault. Geofluids 14:291–309CrossRefGoogle Scholar
  42. Möller P, Rosenthal E, Inbar N, Magri F (2016) Hydrochemical considerations for identifying water from basaltic aquifers: the Israeli experience. J Hydrol Region Stud 5:33–47CrossRefGoogle Scholar
  43. Neev D (1960) A pre Neogene erosion channel in the southern Coastal Plain of Israel. Isr Geol Surv Bull 25:1–21Google Scholar
  44. Picard L (1932) Zur Geologie des Mittleren Jordantales (zwischen Wadi Oschsche und Tiberiassee). Ztschr Dtsch Palest Ver 55:169–236Google Scholar
  45. Picard L (1933) Zur postmiozänen Entwicklungsgeschichte der Kontinentalbecken Nord-Palästinas. Neues Jb Miner 70:93–115Google Scholar
  46. Picard L (1934) Geologischer Beitrag. Zur Geologie des Gebietes zwischen Gilboa und Wadi Fara. Centralbl Miner 1:27–32Google Scholar
  47. Raab M (1996) The origin of evaporates in the Jordan-Arava valley in view of the evolution of brines and evaporates during seawater evaporation. PhD thesis, The Hebrew University of Jerusalem (in Hebrew, English summary), p 114Google Scholar
  48. Rosenthal E (1988a) Hydrogeochemistry of groundwater at unique outlets of the Bet Shean multiple aquifer system. Isr J Hydrol 97:75–87CrossRefGoogle Scholar
  49. Rosenthal E (1988b) Ca-chloride brines at common outlets of the Bet Shean-Harod multiple aquifer system. Isr J Hydrol 97:89–106CrossRefGoogle Scholar
  50. Rouchy JM, Caruso A (2006) The Messinian salinity crisis in the Mediterranean basin: a reassessment of the data and an integrated scenario. Sedim Geol 188–189:35–67CrossRefGoogle Scholar
  51. Rozenbaum AG, Shaked-Geband M, Zilberman E, Sandler A, Stein M, Starinsky A (2016) Depositional environment of the Bira and Gesher Formations of the lower Galilee and Jordan Valley during the Tortonian-Zanclean ages. Geol Soc Isr Ann Meet, Eilat, January 19–21, 2016, Abstract p 171Google Scholar
  52. Salameh E, Al Farajat M (2007) The role of volcanic eruptions in blocking the drainage leading to the Dead Sea formation. Environ Geol 52:519–527CrossRefGoogle Scholar
  53. Salameh E, Rimawi O (1988) Hydrochemistry of precipitation of northern Jordan. Intern J Environ Stud 32:203–216CrossRefGoogle Scholar
  54. Sandler A, Rozenbaum AG, Zilberman E, Stein M, Jicha BR, Singer BS (2015) Updated 40Ar–39Ar chronology for top Lower Basalt, base Cover Basalt, and related units, Northern Valley, Israel. Isr. Geol Soc Ann Meet Kinar, Israel, 24–26 March 2015, p 124Google Scholar
  55. Schulman N (1962) The Geology of the Central Jordan Valley. PhD Thesis, Hebrew University Jerusalem (in Hebrew, English abstract), p 103Google Scholar
  56. Schulman N, Rosenthal E (1968) Neogene and Quaternary of the Marma Feiyad area, south of Bet She’an. Isr J Earth Sci 17:54–62Google Scholar
  57. Shalev E, Yechieli Y (2007) The effect of Dead Sea level fluctuations on the discharge of thermal springs. Isr J Earth Sci 56:19–27CrossRefGoogle Scholar
  58. Shaliv G (1991) Stages in the tectonic and volcanic development of the Neogene basin in northern Israel. PhD Thesis, Hebrew Univ. Jerusalem, English Abstract; Geol Surv Isr Rep GSI/11/91Google Scholar
  59. Shiftan Z, Rosenthal E (1964) Exploratory borehole Hula 2: completion report and comments on regional implications. Geol Surv Isr Rep Hyd/64/3(Hebrew):32Google Scholar
  60. Siebert C, Rosenthal E, Möller P, Rödiger T, Meiler M (2012) The hydrochemical identification of groundwater flowing in the Bet She’an-Harod multiaquifer system (Lower Jordan Valley) by rare earth elements, yttrium, stable isotopes (H, O) and Tritium. Appl Geochem 27:703–714CrossRefGoogle Scholar
  61. Siebert C, Möller P, Geyer S, Kraushaar S, Dulski P, Guttman J (2014) Thermal water in the Lower Yarmouk Gorge and their relation to surrounding aquifers. Chem Erde Geochem 74:425–441CrossRefGoogle Scholar
  62. Siemann MG, Schramm M (2002) Henry’s and non-Henry’s law behavior of Br in simple marine systems. Geochim Cosmochim Acta 68:1387–1399CrossRefGoogle Scholar
  63. Sneh A, Bartov Y, Weissbrod T, Rosensaft M (1998) Geological Map of Israel 1:200,000. Geol. Surv. Isr., Jerusalem, 4 sheetsGoogle Scholar
  64. Starinsky A (1974) Relationships between Ca-chloride brines and sedimentary rocks in Israel. PhD Thesis, Department of Geology, Hebrew University, JerusalemGoogle Scholar
  65. Stein M (2014) The evolution of Neogene-Quaternary water-bodies in the Dead Sea Rift Valley. In: Gafunkel Z, Ben-Avraham Z, Kagan E (eds) Dead Sea Transform fault system: reviews. Springer, Dordrecht, pp 279–316Google Scholar
  66. ten Haven HL, De Lange GJ, Klaver GT (1985) The chemical composition and origin of the Tyro brine, Eastern Mediterranean, a tentative model. Mar Geol 64:337–342CrossRefGoogle Scholar
  67. Warren KC (2008) Salt as sediment in the Central European Basin: system seen as from a deep time perspective. In: Littke R, Bayer U, Gajewski D, Nelskamp S (eds) Dynamics of complex intracontinental basins. Springer, Berlin, pp 249–276Google Scholar
  68. Zak Y (1967) The Geology of Mt. Sdom. PhD Thesis, Department of Geology, Hebrew University Jerusalem, (in Hebrew, English abstract)Google Scholar

Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2018

Authors and Affiliations

  • Peter Möller
    • 1
  • E. Rosenthal
    • 2
  • N. Inbar
    • 2
    • 3
  • C. Siebert
    • 4
  1. 1.Helmholtz Centre PotsdamGerman Research Centre for Geosciences GFZPotsdamGermany
  2. 2.The School of Earth SciencesTel Aviv UniversityTel AvivIsrael
  3. 3.Eastern R&D CenterArielIsrael
  4. 4.Department of Catchment HydrologyUFZ-Helmholtz Centre for Environmental ResearchHalleGermany

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