{"refrec":{"BRefID":32116,"RR":"<b>Rona, P.A.</b> (2003). Resources of the sea floor. <i>Science (Wash.) 299(5607)</i>: 673-674. <a href=\"http://dx.doi.org/10.1126/science.1080679\" target=\"_blank\">http://dx.doi.org/10.1126/science.1080679</a>","BEntID":32116,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 299(5607)</i>: 673-674. <a href=\"http://dx.doi.org/10.1126/science.1080679\" target=\"_blank\">http://dx.doi.org/10.1126/science.1080679</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Rona, P.A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Rona, P.A.","Englishabstract":"In his Perspective, Rona reviews recent advances in knowledge of sea-floor resources. Knowledge is expanding from those minerals eroded from land--metals, gemstones, sand, and gravel--to those minerals concentrated by plate tectonic processes in ocean basins. 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