The rate of change of a soil bacterial community after liming as a function of temperature.
The response of a bacterial community to liming of a forest humus soil (pH 4.9 increased to pH 7.5) was studied in the laboratory at three temperatures (5, 20, and 30 degrees C). As a comparison an unlimed soil (pH 4.9) and a soil limed in the field 15 years ago (pH around 6) were also included. The bacterial community tolerance of pH was measured using TdR incorporation. The pH of the bacterial suspensions (bacteria directly extracted from soil) was altered to 3.6 and 8.3 using different buffers before measuring TdR incorporation. The logarithmic ratio between TdR incorporation at 8.3 and 3.6 was then used as an indicator of the community pH tolerance. The rate of changes in the community tolerance to pH after liming was fastest for the soil incubated at 30 degrees C, but only minor differences in rate of change could be seen between samples incubated at 5 and 20 degrees C. Changes in phospholipid fatty acid (PLFA) pattern after increasing the pH were most rapid for the bacterial community in the soil incubated at 30 degrees C followed by the soil incubated at 20 degrees C, whereas no changes could be seen in the PLFA pattern of the soil incubated at 5 degrees C, even after 82 days' incubation. Thus, the changes in the PLFA pattern were considerably slower than the changes in bacterial community tolerance to pH measured using TdR incorporation.
Pettersson
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M
Department of Microbial Ecology, Ecology Building, Lund University, SE-223 62 Lund, Sweden. Marie.Pettersson@mbioekol.lu.se
Bååth
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E
D000222:Adaptation, Physiological; D001419:Bacteria; D017610:Calcium Compounds; D005227:Fatty Acids / Q000032:analysis / Q000378:metabolism; D006863:Hydrogen-Ion Concentration; D010087:Oxides; D010743:Phospholipids / Q000032:analysis / Q000378:metabolism; D011157:Population Dynamics; D012988:Soil Microbiology; D013696:Temperature; D014197:Trees
D017610:Calcium Compounds; D005227:Fatty Acids; D010087:Oxides; D010743:Phospholipids; C016538:lime