LEADER 02036oam  2200493zu 450 
001 996199870203316
005 20210807004659.0
010   $a1-118-66812-X
035   $a(CKB)3450000000004066
035   $a(SSID)ssj0000815239
035   $a(PQKBManifestationID)11417716
035   $a(PQKBTitleCode)TC0000815239
035   $a(PQKBWorkID)10805974
035   $a(PQKB)11304217
035   $a(NjHacI)993450000000004066
035   $a(PPN)189847921
035   $a(EXLCZ)993450000000004066
100   $a20160829d1993      uy              
101 0 $aeng
135   $aur|||||||||||
181   $ctxt
182   $cc
183   $acr
200 00$aContributions to Antarctic Research III
210 31$a[Place of publication not identified]$cAmerican Geophysical Union$d1993
215   $a1 online resource (ix, 155 pages) $cillustrations
225 1 $aAntarctic research series ;$v57
300   $aBibliographic Level Mode of Issuance: Monograph
311   $a0-87590-825-X 
330   $aPublished by the American Geophysical Union as part of the Antarctic Research Series, Volume 57.Lakes of the dry valley region near McMurdo Sound, Antarctica, which are perennially ice-covered (approximately 4 m thick) and contain only microorganisms in the plankton, present unique systems for studies in hydrologic optics. Profiles of the flux and spectral distribution of photosynthetically available radiation (400-700 nm) and the optical properties of suspended particulate material were measured for Lake Bonney and Lake Fryxell.
410  0$aAntarctic research series ;$v57.
606   $aGeology, Stratigraphic$yCenozoic
606   $aGlacial epoch$zAntarctica
606   $aGravity$zAntarctica$xMeasurement
615  0$aGeology, Stratigraphic
615  0$aGlacial epoch
615  0$aGravity$xMeasurement.
676   $a551.78
702   $aElliot$b David
801  0$bPQKB
906   $aBOOK
912   $a996199870203316
996   $aContributions to Antarctic Research III$92267775
997   $aUNISA