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. 2013 Jul 9;4:181. doi: 10.3389/fmicb.2013.00181

Table 2.

Relative abundances of bGDGTs and bGDGTs-derived proxies for cellulolytic enrichments and natural samples from GBS.

Relative abundance of bGDGTs, normalized to 100% for core bGDGTs and for P-bGDGTs bGDGT proxiesa
I Ib Ic II IIb IIc III MBT CBT TMBT/CBT (°C) pHCBT
Sample Core Polar Core Polar Core Polar Core Polar Core Polar Core Polar Core Polar Core Polar Core Polar Core Polar Core Polar
SEDIMENTS
Site A 56.5 21.5 17.9 24.6 9.0 14.3 9.4 16.4 2.6 2.7 4.6 20.5 0.83 0.60 0.51 0.14 30.9 22.8 7.4 8.4
Site B 50.5 34.3 16.3 15.7 4.3 13.3 16.8 23.3 6.3 0.3 5.7 13.1 0.71 0.63 0.47 0.56 25.1 20.4 7.5 7.3
Site C 72.8 39.1 10.4 12.0 2.6 10.7 8.6 18.0 3.0 8.6 2.7 11.5 0.86 0.62 0.78 0.44 29.4 20.7 6.7 7.6
Site D 46.6 47.4 18.4 17.9 5.8 15.6 17.2 2.2 5.3 11.0 6.8 5.8 0.71 0.81 0.43 0.24 25.3 32.2 7.6 8.1
Site E 72.3 68.1 14.2 9.8 10.5 7.6 1.7 8.6 0.2 2.2 1.2 3.7 0.97 0.86 0.71 0.81 35.7 29.1 6.9 6.6
ENRICHMENT SAMPLES
77AS 90.1 84.3 9.9 15.7
77AW 100.0 100.0
77CS 75.0 56.2 4.6 5.4 25.0 14.9 18.9 0.80 0.56 0.61 28.0 22.0 7.1 8.8
77CW 63.2 52.6 36.8 18.1 29.3
85AS 63.9 42.6 36.1 57.4
85AW 100.0 100.0
85CS 17.7 15.3 28.8 17.0 22.7 15.3 14.1 28.1 11.0 5.4 5.6 19.0 0.69 0.48 0.10 0.29 29.5 15.0 9.0 8.0
85CW 66.2 57.4 33.8 42.6
a

MBT = (I+Ib+Ic)/(I+Ib+ Ic+II + IIb+ IIc + III), in which IIIb and IIIc are all zero values and not included; CBT = −log[(Ib+IIb)/(I+II)]; TMBT/CBT(°C) = (MBT−0.122–0.187*CBT)/0.02; pHCBT = (3.33-CBT)/0.38.

All equations are derived from Weijers et al. (2007a).