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MEDSALT

Uncovering the Mediterranean salt giant

Dissemination meeting – EGU General Assembly 2017, Vienna

egu-logoEuropean Geosciences Union – General Assembly

GEOSCIENCE INFORMATION FOR TEACHERS (GIFT) WORKSHOP Vienna, 23-26 April 2017

Angelo Camerlenghi: UNCOVERING THE MEDITERRANEAN SALT GIANT

Tuesday April 25, 2017 09:15 – 10:00

Gift 2017 Programme

Gift 2017 Abstract Medsalt

Podcast and materials from the GA 2017 GIFT Workshop

Group foto

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News

17 July 2019: The call for the Sixth MEDSALT Short Term Scientific Mission is now open (deadline 15 July 2019)

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

 

 

 

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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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