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Ready for sail­ing - Blo­g­post 1 from RV SONNE, March 5, 2018

San Ant­o­nio, Chile

Fri­day, March 2nd, 2018

Re­search ves­sel SONNE is still moored in the port of San Ant­o­nio at Pier 6. At the be­gin­ning of March on the Pa­cific coast of Chile, sum­mer tem­per­at­ures around 25 de­grees pre­vail. Cap­tain Lutz Mal­lon and his crew await a total of 40 sci­ent­ists from 17 dif­fer­ent parts of the world, in­clud­ing Den­mark, Italy, France, Ger­many, Aus­tria, Spain, Scot­land, Eng­land, Ire­land, Ni­geria, USA, Ja­pan, Canada, China and Taiwan. Ten re­search­ers come from Chile's Uni­ver­sidad de Con­cep­cion and two more from Peru.

Be­fore we leave port, there is a lot more to do. Boxes are be­ing un­packed, equip­ment as­sembled and in­stru­ments checked. There is still time for fi­nal ad­just­ments and re­pairs. For the new­comers on board, an­other chal­lenge is find­ing their way on the 116-meter-long ship. The re­search ves­sel SONNE with ten decks and many labor­at­or­ies can seem like a labyrinth. To make sure that no one gets lost, second of­ficer Lars Hoff­som­mer gives a de­tailed se­cur­ity brief­ing. He also ex­plains what spe­cial rules ap­ply for hu­man in­ter­ac­tion dur­ing the cruise. Where many people get to­gether in a re­l­at­ively small space, it is im­port­ant to take care of each other. For the next weeks, sci­ent­ists and crew will work to­gether to make this ex­ped­i­tion a suc­cess.

Chief Sci­ent­ist Frank Wen­zhöfer from the Max Planck In­sti­tute in Bre­men, Ger­many, co­ordin­ates between the ship's com­mand and the re­search­ers. He sums up the goal of this ex­ped­i­tion: "We will sail to the Atacama Trench, a deep-sea trench that stretches over hun­dreds of naut­ical miles west off the shores of Chile and Peru to a depth of 8000 meters. Our goal is to find out which bio­lo­gical pro­cesses take place in the wa­ter column and in the sed­i­ment. For this, we have many spe­cial­ists on board who brought along an ar­ray of sci­entific equip­ment to take meas­ure­ments and samples. It is im­port­ant to ex­am­ine the ex­tent to which deep-sea trenches act as a sink for car­bon, and which pro­cesses in­flu­ence the car­bon foot­print." The re­search will be co­ordin­ated with Ron­nie Glud from the Uni­versity of South­ern Den­mark in Odense, head of the HADES-ERC pro­ject.

Greet­ings from from the crew and the sci­entific party of So261,

Man­fred Schlösser

Logo der Expedition SO261
The first briefing in the hangar, where scientists present their equipment. Every assignment is planned exactly. Captain Lutz Mallon (second from left) and Chief Scientist Frank Wenzhöfer (right) discuss the technical requirements.
The first briefing in the hangar, where scientists present their equipment. Every assignment is planned in much detail. Captain Lutz Mallon (second from left) and Chief Scientist Frank Wenzhöfer (right) discuss the technical requirements. (Photo: M. Schlösser)
Not to be missed: Alarm exercise in a life jacket
Not to be missed: Alarm exercise in a life jacket. (Photo: M. Schlösser)

Fur­ther in­form­a­tion

More details about the project from the Uni­versity of South­ern Den­mark.

More pictures re­lated to the pro­ject.

Ron­nie N Glud at Dan­marks Radio (in Dan­ish)

RV SONNE is a mod­ern Ger­man re­search ves­sel sail­ing mainly in the Pa­cific Ocean.
More in­form­a­tion about the ship here.

ERC-Logo

Specific questions addressed during this cruise are:

  • What are the sedimentary processes providing food for the hadal community in the Atacama Trench?

  • How do abundance, diversity and community structure of microorganisms, meio- and macrofauna in the Atacama Trench differ from those in less productive trenches and nearby abyssal and shelf sites?

  • What are the general biogeochemical characteristics of the surface and deep sediment and water column in the eutrophic Atacama Trench?

  • Which mineralization pathways are responsible for organic matter breakdown in the eutrophic Atacama Trench?

  • How efficient are microbial communities operating at extreme hydrostatic pressures in mineralizing organic material as compared to their shallower counterparts? And to what extent do specialized, yet unknown extremophile microbial communities mediate these processes?
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