Exploring Europa’s Ocean: A Challenge for Marine Technology of this Century

1999 ◽  
Vol 33 (4) ◽  
pp. 5-12 ◽  
Author(s):  
Frank D. Carsey ◽  
GunShing Chen ◽  
James Cuns ◽  
Lloyd French ◽  
Roger Kern ◽  
...  

The Galileo spacecraft has sent back tantalizing image data hinting at a vast ocean beneath a thick ice crust on Europa, one of Jupiter’s moons which is about the size of our moon. NASA plans to establish definitively whether this ocean exists with the Europa Orbiter mission to be launched in 2003. Should the Europa ocean be a reality, and this looks quite likely, it will mean that another planet besides Earth has an old, deep, salty ocean; the consequences of such an ocean are profound, and there are good reasons to be prepared to take the next step, an in-situ examination of this ocean. A deep subsurface in-situ study of another planetary body has never been attempted, and the challenges are considerable. In this paper we address the technology to be developed to be ready for this exciting mission, and we seek to initiate the exchanges needed between the marine technology and space exploration communities.

2020 ◽  
Vol 9 (1) ◽  
pp. 64
Author(s):  
Maija Nuppunen-Puputti ◽  
Riikka Kietäväinen ◽  
Lotta Purkamo ◽  
Pauliina Rajala ◽  
Merja Itävaara ◽  
...  

Fungi have an important role in nutrient cycling in most ecosystems on Earth, yet their ecology and functionality in deep continental subsurface remain unknown. Here, we report the first observations of active fungal colonization of mica schist in the deep continental biosphere and the ability of deep subsurface fungi to attach to rock surfaces under in situ conditions in groundwater at 500 and 967 m depth in Precambrian bedrock. We present an in situ subsurface biofilm trap, designed to reveal sessile microbial communities on rock surface in deep continental groundwater, using Outokumpu Deep Drill Hole, in eastern Finland, as a test site. The observed fungal phyla in Outokumpu subsurface were Basidiomycota, Ascomycota, and Mortierellomycota. In addition, significant proportion of the community represented unclassified Fungi. Sessile fungal communities on mica schist surfaces differed from the planktic fungal communities. The main bacterial phyla were Firmicutes, Proteobacteria, and Actinobacteriota. Biofilm formation on rock surfaces is a slow process and our results indicate that fungal and bacterial communities dominate the early surface attachment process, when pristine mineral surfaces are exposed to deep subsurface ecosystems. Various fungi showed statistically significant cross-kingdom correlation with both thiosulfate and sulfate reducing bacteria, e.g., SRB2 with fungi Debaryomyces hansenii.


2021 ◽  
Vol 27 (S1) ◽  
pp. 1554-1555
Author(s):  
Chen Gu ◽  
Nabil Bassim ◽  
Hatem Zurob

2021 ◽  
Vol 92 (4) ◽  
pp. 045106
Author(s):  
R. I. Kosheleva ◽  
T. D. Karapantsios ◽  
M. Kostoglou ◽  
A. Ch. Mitropoulos

Author(s):  
Albert Grau-Carbonell ◽  
Sina Sadighikia ◽  
Tom A. J. Welling ◽  
Relinde J. A. van Dijk-Moes ◽  
Ramakrishna Kotni ◽  
...  

Materialia ◽  
2021 ◽  
Vol 15 ◽  
pp. 101033
Author(s):  
Sandra Ebner ◽  
Ronald Schnitzer ◽  
Emad Maawad ◽  
Clemens Suppan ◽  
Christina Hofer

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