Table 3.
Total number of prokaryotes in unconsolidated subsurface sediments
Depth interval,* m | Cells/cm3, × 106 | No.
of cells, × 1028
|
||
---|---|---|---|---|
Deep oceans† | Continental shelf and slope‡ | Coastal plains§ | ||
0.1 | 220.0¶ | 66.0 | 14.5 | 4.4 |
10 | 45.0¶ | 121.5 | 26.6 | 8.1 |
100 | 6.2¶ | 18.6 | 4.1 | 1.2 |
200 | 19.0¶ | 57.0 | 12.5 | 3.8 |
300 | 4.0¶ | 12.0 | 2.6 | 0.8 |
400 | 7.8¶ | 10.1 | 3.2 | |
600 | 0.95‖ | 3.7 | 1.2 | |
1,200 | 0.61‖ | 3.2 | 1.0 | |
2,000 | 0.44‖ | 2.6 | 0.9 | |
3,000 | 0.34‖ | 0.7 | ||
Total | 275.1 | 79.9 | 25.3 | |
Grand Total: 380 × 1028 = 3.8 × 1030 |
Depth intervals are designated by the upper boundary. Thus, “0.1” represents 0.1–10 m and “3,000” represents 3,000–4,000.
Corresponds to seismic layer I (23).
Corresponds to subcontinental sediments (23).
Corresponds to geosyncline sediments of Mesocenozoic origin (23).
Calculated from the arithmetic averages.
Calculated by extrapolation of the formula of Parkes et al. (33).