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. 2002 Jun;68(6):3085–3093. doi: 10.1128/AEM.68.6.3085-3093.2002

TABLE 1.

Characteristics of Fe mats at Loihi, including total number of cells and oxide morphotypee

Sample location Sample no. Depth (m below sea level) Temp (°C)a Mat density (g/ml) Total Fe (mg/g [dry wt]) No. of cells (SD)b Dilution seriesc Dominant morphotype(s)d
Pele's Pit, Ikaika vents, marker 20 393, 1-4 1,317 68 0.170 55 2.93 × 108 (4.2 × 107) 10−4 Filaments
Pele's Pit, Ikaika vents, lower jets 393, 5-8 1,298 167 0.268 81 6.9 × 107 (1.6 × 107) 10−7 Amorphous
South rift, Naha vents, marker 1 396, 2-4 1,325 10 0.097 183 2.45 × 108 (7.94 × 107) 10−6 (10−4 at 12°C) Filaments
Upper South rift, Pohaku vents, marker 27 396, 6 1,196 17 0.049 77 9.33 × 107 (8.6 × 106) 10−5 Amorphous, sheaths
Upper South rift, Pohaku vents, marker 27 396, 7-8 1,196 17 0.157 153 1.26 × 108 (3.1 × 107) 10−7 Amorphous, filaments
Pele's Pit, Ikaika vents, lower jets 397, 1-4 1,295 165 0.140 141 4.61 × 108 (6.5 × 107) 10−6 Amorphous
Pele's Pit, Ikaika vents, upper jets 397, 5 1,289 167 ND ND ND ND Amorphous
Pele's Pit, Ikaika vents, near marker 15 398, 5-6 1,290 113 0.115 152 1.54 × 108 (4 × 107) 10−6 Amorphous, filaments
a

All temperatures are the maximums measured in the vent orifice closest to the sampling site.

b

These values are expressed per milliliter (wet weight) of mat.

c

The highest dilution in a series that yielded growth.

d

The predominant iron oxide morphotypes (Fig. 4 and 5).

e

ND, not determined.