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Therefore we suggest a best estimate of Indonesian peat carbon of 28.1 GtC, the midpoint of the medium estimates of the two map sources.
Medium estimates assumed the depth of all peatlands within a given class were at the midpoint (i.e. 150 cm used for the 100 200 cm depth class), and high estimates assumed all peatlands within a given depth class were the highest end of the class (i.e. 200 cm used for the 100 200 cm interval).
The medium estimates of 25.3 and 30.8 GtC obtained from the MoA and WI maps (respectively) are substantially lower than those of Page et al. [2] and Jaenicke et al. [13] but are closer to the cumulative total of Wahyunto et al.'s [5 7] values available for the WI maps (37.2 GtC).
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Similarly, 14.77 GtC are estimated in depth classes >400 cm on the WI maps; about 48% of the 30.79 GtC medium estimate.
Using a refined modeling approach, Dommain et al. [9] quantified carbon stocks of West Indonesia (Sumatra and Kalimantan) at about 23 GtC, close to our 24.7 GtC medium estimate using the WI maps for the same area.
The low estimate, 300 cm, is the upper end of depth reported by the MoA maps; the high estimate is the midpoint of the 800 1200 cm deepest depth class used in the WI maps (Kalimantan) and the medium estimate is the midpoint of the 300 cm minimum and 1200 cm maximum reported for the deepest depth class in the MoA and WI (Kalimantan) maps respectively.
As a medium estimate, we took an approximate average of these percentages, assuming that large whales constitute 25% of historical numbers and small cetaceans 50%.
Bacteria were resuspended in M63A buffered with 5 mM HOMOPIPES at pH 7.5, a medium estimated to contain less than 10 mM K+.
Taking the HPS-based multiplier as the medium estimate, the low and the high estimates were generated by adding and subtracting one, respectively, from the medium estimate.
The medium estimate based on the national multiplier indicates that an estimated 464,000 induced abortions occurred in Kenya in 2012.
Growth rates of E. coli cultured in batch in TSB medium estimated based on OD600 measurements decreased continuously until the stationary phase and the maximum difference during the initial 3 hours was ca 1.7 h−1.7
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