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MEDSALT

Uncovering the Mediterranean salt giant

MedSalt Symposium – Palermo, 24-28 October 2016

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Program

Presentations

Press release

ECORD Newsletters, N. 28, April 2017

Multimedia

Pictures

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News

18 December 2018: The call for the “Training School 3: The Messinian Salinity Crisis from a fieldwork perspective” is now open (deadline 15 January 2019)

27-28-29 November 2018: MEDSALT Action presented at the Annual Congress of the Academia Europaea and the young Academy of Europe (Barcelona)

5 November 2018: The call for the Fifth MEDSALT Short Term Scientific Mission is now open (deadline 30 November)

9-10 October 2018: 4th MEDSALT Management Committee Meeting and Working Group meeting in Belgrade

4 May 2018: Open letter on behalf of MEDSALT  network (English version) – Comunicado en nombre de la red de científicos europeos (MEDSALT) (Spanish version)

3 May 2018: Medsalt-2 solicitud 2018

27 April 2018: The call for the Fourth Short Term Scientific Mission is now open

9 April 2018: COST Actions in Geosciences at EGU General Assembly 2018, Vienna

 

 

 

Events

  • COST Connect Oceans Brussel 13 June 2019 – 14 June 2019
  • SALTGIANT Event Trieste 17 June 2019 – 26 June 2019

Video Palermo Symposium

COST is supported by the EU Framework Programme Horizon 2020

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Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Training School 1: Seismic interpretation applied to salt basins in different geodynamic settings (Cyprus, September 2017)
Gypsum crust from the bottom of a shallow saltern pond (200 g l−1 salinity) in Eilat, Israel, showing layered communities of phototrophic microbes. The orange-brown upper layer is dominated by unicellular cyanobacteria and the green layer by filamentous cyanobacteria; and the red-purple layer contains a dense community of purple sulfur bacteria (e.g. Halochromatium spp.) that oxidize sulfide produced by sulfate-reducing bacteria present in the lower grey layer, © Andreas Thywißen. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
Gypsum crust from the bottom of a shallow saltern pond (200 g l−1 salinity) in Eilat, Israel, showing layered communities of phototrophic microbes. The orange-brown upper layer is dominated by unicellular cyanobacteria and the green layer by filamentous cyanobacteria; and the red-purple layer contains a dense community of purple sulfur bacteria (e.g. Halochromatium spp.) that oxidize sulfide produced by sulfate-reducing bacteria present in the lower grey layer, © Andreas Thywißen. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
The red pond on the left is saturated with NaCl, and has a visible halite crust. The mound of harvested salt is about 2.5 m high, © Rafael Bosch. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
The red pond on the left is saturated with NaCl, and has a visible halite crust. The mound of harvested salt is about 2.5 m high, © Rafael Bosch. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
Microscopic image from a natural hypersaline brine (salinity > 200 g l−1). Based on distinctive morphologies the following can be identified: the eukaryotic green alga Dunaliella salina living alongside the haloarchaeon Haloquadratum walsbyi (flat square with gas vesicles; numerous cells are dividing like a sheet of postage stamps). A rod-shaped microbe can also be seen, © Mike Dyall-Smith. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
Microscopic image from a natural hypersaline brine (salinity > 200 g l−1). Based on distinctive morphologies the following can be identified: the eukaryotic green alga Dunaliella salina living alongside the haloarchaeon Haloquadratum walsbyi (flat square with gas vesicles; numerous cells are dividing like a sheet of postage stamps). A rod-shaped microbe can also be seen, © Mike Dyall-Smith. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
Scanning electron micrograph of Halococcus salifodinae strain BIp, isolated from a salt mine in Austria, © Gerhard Wanner. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
Scanning electron micrograph of Halococcus salifodinae strain BIp, isolated from a salt mine in Austria, © Gerhard Wanner. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
Laboratory-made crystals of NaCl encasing the haloarchaeon, Halorubrum saccharovorum. The cloudiness of the halite (NaCl) crystals is due to the large number of brine inclusions. Each crystal is ca. 1 cm square, © Terry J. McGenity. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
Laboratory-made crystals of NaCl encasing the haloarchaeon, Halorubrum saccharovorum. The cloudiness of the halite (NaCl) crystals is due to the large number of brine inclusions. Each crystal is ca. 1 cm square, © Terry J. McGenity. (For more details see: McGenity TJ & Oren A (2012) Hypersaline environments. In Life at Extremes: Environments, Organisms and Strategies for Survival. EM Bell (ed.) CAB International, UK. pp. 402-437)
Medsalt OGS Explora Cuise, Baleares July 2015 (credits Angelo Camerlenghi)
Medsalt OGS Explora Cuise, Baleares July 2015 (credits Angelo Camerlenghi)
Medsalt OGS Explora Cuise, Baleares July 2015 (credits Angelo Camerlenghi)
Medsalt OGS Explora Cuise, Baleares July 2015 (credits Angelo Camerlenghi)
Medsalt OGS Explora Cuise, Baleares July 2015 (credits Angelo Camerlenghi)
Medsalt OGS Explora Cuise, Baleares July 2015 (credits Angelo Camerlenghi)
Medsalt OGS Explora Cuise, Baleares July 2015 (credits Angelo Camerlenghi)
Sampling intercalated clays within the Sorbas (SE. Spain) Messinian peripheral primary gypsum Popescu-Suc (credits Marcello Natalicchio)
Sampling intercalated clays within the Sorbas (SE. Spain) Messinian peripheral primary gypsum Popescu-Suc (credits Marcello Natalicchio)
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