Primary production of the cryptoendolithic microbiota from the Antarctic Desert.
Primary production in the Antarctic cryptoendolithic microbiota can be determined from biomass and photosynthetic 14CO2 incorporation measurements.  Even though good nanoclimate data are available, it is difficult to determine the amount of time when abiotic conditions permit metabolism.  Making appropriate assumptions concerning the metabolism of the cryptoendolithic microbiota during periods of warmth, light and moisture, the primary production of the biota was calculated to be on the order of 0.108 to 4.41 mgC/m2/yr, with a carbon turnover time from 576 to 23,520 years.  These production values are the lowest found on planet Earth.
Vestal
J R
JR
Department of Biological Sciences, University of Cincinnati, OH 45221-0006, USA.
D000864:Antarctic Regions; D018533:Biomass; D002244:Carbon / Q000032:analysis / Q000378:metabolism*; D002250:Carbon Radioisotopes; D002980:Climate; D017753:Ecosystem; D008011:Lichens / Q000378:metabolism* / Q000502:physiology; D008027:Light; D010788:Photosynthesis / Q000502:physiology; D013696:Temperature; D014867:Water
D002250:Carbon Radioisotopes; D014867:Water; D002244:Carbon