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dc.contributor.authorHolm, Nils G.
dc.contributor.authorCairns-Smith, Graham
dc.contributor.authorDaniel, Roy M.
dc.contributor.authorFerris, James P.
dc.contributor.authorHennet, Remy J.-C.
dc.contributor.authorShock, Everett L.
dc.contributor.authorSimoneit, Bernd R.T.
dc.contributor.authorYanagawa, Hiroshi
dc.date.accessioned2010-08-31T00:34:33Z
dc.date.available2010-08-31T00:34:33Z
dc.date.issued1992
dc.identifier.citationHolm, N.G., Cairns-Smith, G., Daniel, R.M., Ferris, J.P., Hennet, R.J.C., …, Yanagawa, H. (1992). Future research. Origins of Life and Evolution of Biospheres, 22(1-4), 181-190.en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/4480
dc.description.abstractWhat field studies need to be carried out in order to test the hydrotherrnal model for the origin of life? This question was already raised in 1989 by the workshop in Prague on 'Chemical Evolution and Neo-Abiogenesis in Marine Hydrothermal Systems' (Holm, 1990). The full range and diversity of hydrothermal environments can only be revealed if more exploration work is carried out on a world-wide basis. Much progress has been made in understanding the controls on the hydrothermal fluids of individual areas, but extension to a global context remains difficult (cf. Von Datum, 1990). In Chapter 2 off-axis hydrothermal systems are discussed, pointing out that only minor surveys have been directed towards this type of hydrothermal activity, even though the amount of water which circulates through off-axis systems is estimated to exceed that of on-axis systems by a factor of between 20 and 25.en_NZ
dc.language.isoen
dc.publisherSpringeren_NZ
dc.relation.urihttp://www.springerlink.com/content/r2723n14r5k56713/en_NZ
dc.subjectnatural systemen_NZ
dc.titleFuture researchen_NZ
dc.typeJournal Articleen_NZ
dc.identifier.doi10.1007/BF01808024en_NZ


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