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. 2014 May 7;5:202. doi: 10.3389/fmicb.2014.00202

Table 2.

Properties of various Pseudomonas sp. strains examined.

Strain Pseudomonas species or group (gp), from 16S rRNAa Forms MnO2 CAS reactionb (PVD reaction)b Sidero-typec 59Fe-PVD uptake (% of homologous uptake)d Isolated frome (references in footnote)
CFML 90-45 putida No CAS+ (PVD+) 1 CFML 90-51 (>90%) Clinical specimen
CFML 90-48 putida No CAS+ (PVD+) 1 CFML 90-51 (>90%) Clinical specimen
CFML 90-49 putida No CAS+ (PVD+) 1 CFML 90-51 (>90%) Clinical specimen
CFML 90-50 putida No CAS+ (PVD+) 1 CFML 90-51 (>90%) Clinical specimen
CFML 90-51 putida No CAS+ (PVD+) 1 CFML 90-51 (100%) Clinical specimen
GB-1 putida Yes CAS+ (PVD+) 1 CFML 90-51 (95%) Freshwater sediment
MnB1 putida Yes CAS+ (PVD+) 1 CFML 90-51 (104%) Freshwater pipe
KT2440 putida Yes, at low O2 CAS+ (PVD+) 2 F317 (91%) Soil, toluate deg
ATCC 55241 fluorescens biotype II BNL-WVC No CAS+ (PVD+) 3 No match to known PVD Radiowaste leachate
ISO6 fluorescens-syringae gp. Yes, at low O2 CAS+ (PVD+) 4 Metallogenium particles
PCP1 fluorescens-syringae gp. Yes CAS+ (PVD+) 4 D47, SB8.3 (~50% each) Sediment, mine drainage
MG1 fluorescens-syringae gp. Yes CAS+ (PVD+) NTf Metallogenium particles
ISO1 fluorescens-syringae gp. Yes CAS+ (PVD−) NAg Metallogenium particles
GP11 stutzeri gp. Yes CAS− (PVD−) NA Pulpmill effluent
SI85-2B marincola Yes CASNT (PVD−) NA Marine bay, suboxic
PCP2 mendocina-resinovorans gp. Yes CAS− (PVD−) NA Sediment, mine effluent
a

Based on 16S rRNA sequence (Francis and Dodge, 1998; Francis and Tebo, 2001; Meyer et al., 2007).

b

The chrom azurol S (CAS) method, which depends on the ability of siderophores to displace Fe from its CAS complex, is a general assay for siderophores (Schwyn and Neilands, 1987). The presence of pyoverdine-group siderophores (PVD) was detected from UV-vis absorption and fluorescence spectra (Parker et al., 2007). A strain was scored positive (+) if a CAS reaction or PVD was detected.

c

Based on the isolectric focusing pattern of each strain's fluorescent PVD and confirmed by each strain's uptake of 59Fe-PVD from 34 standard strains, using methods in Fuchs et al. (2001), but with assigning of our own siderotype numbers.

d

FePVD standard that was taken up in greatest amount. (% uptake compared to that of the homologous standard strain).

e

Clinical specimen or from associated medical environment, Collection de la Faculté de Médecine de Lille, France (Meyer et al., 2007); freshwater pipe encrusted with MnO2, Germany (Schweisfurth, 1973); freshwater sediment, Green Bay of Lake Michigan, USA (Francis and Tebo, 2001); laboratory variant selected by Brandy Toner in the Garrison Sposito laboratory, University of California Berkeley, USA; marine fjord, oxic-anoxic interface, Saanich Inlet, Vancouver Island, BC, Canada (Emerson et al., 1982; Francis and Tebo, 2001; Romanenko et al., 2008); Metallogenium particles from Horsetooth Reservoir, Fort Collins, CO, USA (Francis and Tebo, 2001); pulpmill effluent, Grande Prairie, AB, Canada (Francis and Tebo, 2001); radiowaste leachate, low-level radioactive waste leachate, Brookhaven Natl. Lab., USA (Francis and Dodge, 1998); sediment, mine drainage, Pinal Creek, Globe, AZ, USA, downstream from a Cu mine (Fuller and Harvey, 2000; Francis and Tebo, 2001); soil, toluate deg, soil enrichment for degradation of toluate, Osaka, Japan (Nakazawa, 2002; Regenhardt et al., 2002).

f

NT, not tested. Strain MG-1 did not grow at the standard conditions used for IEF analysis and 59Fe PVD uptake.

g

NA, not applicable because that organism does not make PVD.