LEADER 00929nam0-22003251i-450- 001 990003705080403321 005 20110301111030.0 010 $a0521351057 035 $a000370508 035 $aFED01000370508 035 $a(Aleph)000370508FED01 035 $a000370508 100 $a20030910d1992----km-y0itay50------ba 101 0 $aita 105 $ay-------001yy 200 1 $aDisarray in world food markets$ea quantitative assessment$fRod Tyers and Kym Anderson 210 $aCambridge$cCambridge University Press$d1992 215 $aXXIV, 444 p.$d22 cm 225 1 $aTrade and development 700 1$aTyers,$bRod$0140585 702 1$aAnderson,$bKym 801 0$aIT$bUNINA$gRICA$2UNIMARC 901 $aBK 912 $a990003705080403321 952 $aQ1.101$b6402$fDECTS 952 $aH/1.21 TYE$b11824$fSES 959 $aDECTS 959 $aSES 996 $aDisarray in world food markets$9500883 997 $aUNINA LEADER 02880nam 2200433z- 450 001 9910261138303321 005 20210212 035 $a(CKB)4100000002484709 035 $a(oapen)https://directory.doabooks.org/handle/20.500.12854/57731 035 $a(oapen)doab57731 035 $a(EXLCZ)994100000002484709 100 $a20202102d2017 |y 0 101 0 $aeng 135 $aurmn|---annan 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 00$aRecent Advances in Geomicrobiology of the Ocean Crust 210 $cFrontiers Media SA$d2017 215 $a1 online resource (328 p.) 225 1 $aFrontiers Research Topics 311 08$a2-88945-283-2 330 $aIgneous oceanic crust is one of the largest potential habitats for life on earth, and microbial activity supported by rock-water-microbe reactions in this environment can impact global biogeochemical cycles. However, our understanding of the microbiology of this system, especially the subsurface "deep biosphere" component of it, has traditionally been limited by sample availability and quality. Over the past decade, several major international programs (such as the Center for Dark Energy Biosphere Investigations, the current International Ocean Discovery Program and its predecessor Integrated Ocean Drilling Program, and the Deep Carbon Observatory) have focused on advancing our understanding of life in this cryptic, yet globally relevant, biosphere. Additionally, many field and laboratory research programs are examining hydrothermal vent systems -a seafloor expression of seawater that has been thermally and chemically altered in subseafloor crust - and the microbial communities supported by these mineral-rich fluids. The Frontiers in Microbiology 3 September 2017 | Recent Advances in Geomicrobiology of the Ocean Crust papers in this special issue bring together recent discoveries of microbial presence, diversity and activity in these dynamic ocean environments. Cumulatively, the articles in this special issue serve as a tribute to the late Dr. Katrina J. Edwards, who was a pioneer and profound champion of studying microbes that "rust the crust". This special issue volume serves as a foundation for the continued exploration of the subsurface ocean crust deep biosphere. 606 $aMicrobiology (non-medical)$2bicssc 610 $adeep biosphere 610 $aGeomicrobiology 610 $ahydrothermal vents 610 $aIODP 610 $airon oxidation 610 $aocean crust 610 $asulfate reduction 615 7$aMicrobiology (non-medical) 700 $aJason B. Sylvan$4auth$01320422 702 $aCara M. Santelli$4auth 702 $aBeth N. Orcutt$4auth 906 $aBOOK 912 $a9910261138303321 996 $aRecent Advances in Geomicrobiology of the Ocean Crust$93034288 997 $aUNINA