Lozupone and Knight. 10.1073/pnas.0611525104.
Fig. 4. UniFrac UPGMA cluster. The results of clustering the 202 samples by using a UniFrac distance matrix and the UPGMA algorithm. The nonsaline environments form a monophyletic clade (denoted with two blue stars) that separates them from the saline environments. The branches are colored by environment type with the following colors: Nc, yellow; Nso, light green; Nsu, red; Nse, purple; Nw, blue; Nen, salmon; Nsp,: brown; Sc, yellow; Sse, orange; Swa, bright green; Swb, dark blue; Sws, cyan; Smi, light purple; So, hot pink; M, black. The groups indicated by boxes on the right (and a red star for the clade where applicable) are described in more detail below. A file with the sample names associated with each branch ("UPGMA_results.html") is also provided. A, saline sediment, anoxic water, and misc other: Two hydrothermal sediments from the Saline sediment (Sse) group (Sse_Mh_42, Sse_Mh_18), anoxic water (Swa_M_32, Swa_M_33), and members of the Saline-Misc group (So) including hypersaline microbial mats (So_Mm+_166-8) and hydrothermal vent colonizers (So_Hc_19, So_Hc_128). B, Subsurface and open ocean water: All members of the Saline water submerged (Swb) group except for Swb_M_130 (which groups with the surface water) and two members of Saline water surface (Sws) group, Sws_M_83 and Sws_M_163. C, Saline sediment, anoxic water, and misc other: Diverse samples from the Saline sediment (Sse) group, five samples from anoxic hypersaline basins in the Mediterranean Sea (Swa group), and a couple of members of the Saline-Misc group (So). D, Saline sediment and misc other: Diverse samples from the Saline sediment (Sse) group and from the Saline-Misc group (So) including all four stromatolite samples, formations in a cave flooded with saline groundwater (So_36), basalt from the seafloor (So_En_135), and salt march grass (So_Mc_72). E, Saline sediment/anoxic: Mostly sediments but also anoxic water from a saline lake (Swa_L+_59). F, Coastal surface water: Most members of the Saline water surface (Sws) group, two estuary water samples (M_w_200, M_w_201), and one member of the Saline water subsurface (Swb) group (Swb_M_130) form a clade with the Saline Cultured (Sc) group members. G, Saline-cultured and Marine Ice: All but one member of the Saline Cultured (Sc) group (Sc_Mr+_84, from a stromatolite, groups closer to the uncultured stromatolite samples) and all members of the Marine Ice (Smi) group. H, Misc and submerged soils: Miscellaneous members of the soil (Nso) group and most member of the Non-saline submerged (Nsu) group including wetlands, aquifers, and a rice paddy. I, Nonsaline sediment: All members of the Nonsaline sediment (Nse) group. J, Soil: Most members of the soils (Nso) group. K, Rock and Cave: Members of the Nonsaline endolithic group (Nen), two of four from caves, and sediment from aphotic wind cave in South Dakota (N_su_c_188). L, Misc nonsaline: Miscellaneous members of the Nonsaline endolithic (Nen), Soil (Nso), and submerged soils (Nsu) groups, that group in a clade with members of the Nonsaline cultured (Nc) group, including extremely acidic rocks in Yellowstone National Park (Nen_100) and PCB contaminated soils (Nso_p_23, Nso_p_34). M, Nonsaline cultured: Members of the Nonsaline cultured (Nc) group that were cultured from soils, sediments, and air. One member of the Nonsaline endolithic (Nen) group (Nen_110) N: Lakes and Rivers: All samples in the Nonsaline water (Nw) group, all lake samples in the Nonsaline-cultured (Nc) group, one estuary (M_w_11), and one Saline water-surface sample (Sws_M_13). Sws_M_13 was likely pulled into this group because it is from a single study that sequenced from a river, estuary, and adjacent coastal ocean, which all group in this clade. O, Hotsprings: All hotsprings in the Nonsaline springs (Nsp) group and an intertidal hotspring (M_sp_101) from the Mixed (M) group.
Fig. 5. Phylogenetic diversity (PD) regression analysis. Plot of the amount of branch length that remains in the phylogenetic tree when only sequences from a particular sample is included (PD), vs. the number of OTUs that represents each sample. Bacteria that were cultured from nonsaline environments (Nc, pink circles) generally fell below the main regression line (blue), thus having lower phylogenetic diversity. Saline sediments (purple circles) generally fell above the main regression line.
Data Set 1. Information on the environmental samples that are included in the survey
|
Name |
Description |
# SEQ |
# OTU |
G Resid |
PD Resid |
Ref |
|
M_sp_101 |
Intertidal hotsprings on the coast of the Reykjanes peninsula in northwest Iceland (45-95C) |
38 |
33 |
0.206 |
1.145 |
1 |
|
M_w_11 |
Columbia River Estuary, Oregon, |
119 |
82 |
-0.785 |
1.293 |
2 |
|
M_w_200 |
Station N1 of the Portuguese estuary Ria de Aveiro representing a deep marine zone |
32 |
31 |
-0.474 |
-0.914 |
3 |
|
M_w_201 |
Station I6 of the Portuguese estuary Ria de Aveiro representing a shallow brackish zone |
25 |
24 |
-0.261 |
-0.318 |
3 |
|
Nc_ai_132 |
Aerosolized bacteria from desert dust events in Mali, West Africa (cultured) |
95 |
48 |
-0.874 |
-3.051 |
4 |
|
Nc_Ls_97 |
Cultured from sediment from shallow, eutrophic Lake Kasumigaura in Japan |
210 |
66 |
-0.772 |
-0.555 |
5 |
|
Nc_Lw_113 |
Cultured from water from small, shallow, eutrophic lake Zwischenahner Meer in Northern Germany |
43 |
24 |
-0.418 |
-0.746 |
6 |
|
Nc_Lw_114 |
Cultured from water from mesotrophic prealpine lake Starnberger, Southern Bavaria, Germany |
36 |
23 |
-0.399 |
-0.817 |
6 |
|
Nc_Lw_115 |
Cultured from water from oligotrophic alpine lake Walchensee, Southern Bavaria, Germany |
33 |
16 |
-0.349 |
-1.118 |
6 |
|
Nc_so_186 |
Cultured from sand from the desert of Tataouine (south Tunisia) |
40 |
25 |
-0.235 |
-1.481 |
7 |
|
Nc_so_39 |
Cultured from no-tilled agricultural soil in Athens, Georgia |
73 |
59 |
-1.253 |
-3.034 |
8 |
|
Nc_so_40 |
Cultured from an earthworm burrow in no-tilled agricultural soil in Athens, Georgia |
26 |
21 |
-0.431 |
-1.628 |
8 |
|
Nc_so_73 |
Cultured from a grass pasture soil in Victoria. England |
350 |
95 |
-1.488 |
-2.729 |
9 |
|
Nc_so_82 |
Cultured from a pasture soil in Victoria, Australia |
89 |
46 |
-0.899 |
-1.881 |
10 |
|
Nc_so_95 |
Cultured from a pasture soil from Victoria, Australia |
258 |
122 |
-2.531 |
-3.393 |
11 |
|
Nen_100 |
Extremely acidic (pH 1) rocks in the geothermal environment of Yellowstone National Park |
65 |
42 |
0.618 |
0.913 |
12 |
|
Nen_110 |
Wall of aphotic, oligotrophic Fairy Cave in Colorado (U.S.A.) |
37 |
31 |
0.189 |
-0.419 |
13 |
|
Nen_126 |
Wall of aphotic La Garma Cave, northern Spain |
58 |
39 |
-0.327 |
-0.456 |
14 |
|
Nen_127 |
Wall of artificially lighted Llonin Cave, northern Spain |
27 |
17 |
0.120 |
-0.595 |
14 |
|
Nen_192 |
Epilithic bacterial community in Limestone from a Maya archaeological site in Yucatan Mexico |
54 |
49 |
0.699 |
1.527 |
15 |
|
Nen_193 |
Endolithic bacterial community in Limestone from a Maya archaeological site in Yucatan Mexico |
30 |
28 |
0.087 |
-0.590 |
15 |
|
Nen_45 |
Wall of artificially lighted Tito Bustillo cave, Spain |
41 |
33 |
0.025 |
-0.119 |
16 |
|
Nse_L_149 |
Sediment from Rainbow Bay, an acidic, mesotrophic freshwater pond on the Carolina coastal plain (U.S.A.) |
33 |
31 |
0.392 |
-0.417 |
17 |
|
Nse_L_150 |
Sediment from oligotrophic, acidic Muldenberg reservoir, Saxony Germany |
164 |
142 |
0.727 |
2.449 |
18 |
|
Nse_L_151 |
Sediment from oligotrophic Neuzehnhain rezervoir, Saxony Germany |
158 |
137 |
0.302 |
1.542 |
18 |
|
Nse_L_152 |
Sediment from highly eutrophic Quitzdorf rezervoir, Saxony Germany |
145 |
133 |
1.618 |
4.013 |
18 |
|
Nse_L_153 |
Sediment from mesotrophic Saidenbach rezervoir, Saxony Germany |
147 |
128 |
1.498 |
4.022 |
18 |
|
Nse_L_198 |
Sediment of freshwater Lake Washington (60m depth) |
104 |
54 |
-0.476 |
0.473 |
19 |
|
Nse_L_98 |
Sediment from shallow, eutrophic Lake Kasumigaura in Japan |
112 |
83 |
0.133 |
0.371 |
5 |
|
Nso_10 |
Rhizosphere samples from fertilized and reseeded grass pasture soils in Scotland |
137 |
116 |
-1.276 |
0.831 |
20 |
|
Nso_106 |
Light, sandy loam soil in arid northern Arizona, U.S.A. |
254 |
200 |
0.173 |
0.139 |
21, 22 |
|
Nso_107 |
Coarse textured, well-drained cinder soil in arid northern Arizona U.S.A. |
286 |
182 |
-0.574 |
-0.696 |
21, 22 |
|
Nso_108 |
Agricultural soil in Wisconsin U.S.A. |
526 |
351 |
-1.406 |
-3.027 |
23 |
|
Nso_116 |
Rhizosphere of lodgepole pine seedlings in Williams Lake, British Columbia |
226 |
179 |
-2.330 |
-1.047 |
24 |
|
Nso_117 |
Rhizosphere of lodgepole pine seedlings in Smithers, British Columbia |
211 |
170 |
-2.142 |
-1.025 |
24 |
|
Nso_118 |
Rhizosphere of lodgepole pine seedlings in Prince George, British Columbia |
217 |
160 |
-2.388 |
-0.996 |
24 |
|
Nso_158 |
Sandy soil in Virginia, U.S.A. |
67 |
48 |
-0.479 |
0.480 |
25 |
|
Nso_159 |
Sandy soil in Delaware, U.S.A. |
75 |
46 |
0.072 |
-0.392 |
25 |
|
Nso_185 |
Sand from the desert of Tataouine (south Tunisia) |
117 |
91 |
0.133 |
0.882 |
7 |
|
Nso_190 |
Loamy-sand soil from a chaparral ecosystem in San Diego, California U.S.A. |
126 |
92 |
-0.475 |
0.264 |
26 |
|
Nso_199 |
Soil from exotic pine plantations of subtropical Australia under different residue management regimes |
314 |
190 |
-1.103 |
-3.392 |
27 |
|
Nso_202 |
Silt loam soil from a century-old manure treated agroecosystem in Oklahoma, U.S.A. |
94 |
61 |
-0.375 |
0.646 |
28 |
|
Nso_3 |
Agricultural soil in Wisconsin, U.S.A. |
120 |
116 |
0.198 |
-0.665 |
29 |
|
Nso_4 |
Mature forest and active pasture soils in Para State Brazil |
99 |
86 |
0.851 |
1.214 |
30 |
|
Nso_41 |
No-tilled agricultural soil in Athens, Georgia |
95 |
84 |
0.200 |
1.744 |
8 |
|
Nso_46 |
Forest soil in British Columbia after whole tree harvesting with no soil compaction |
280 |
205 |
-2.050 |
-0.853 |
31 |
|
Nso_47 |
Forest soil in British Columbia after whole tree harvesting and surface organic matter removal |
140 |
118 |
-1.291 |
0.579 |
31 |
|
Nso_65 |
Uncultivated agricultural soil in Wisconsin |
318 |
249 |
-0.852 |
-4.308 |
32 |
|
Nso_79 |
Tropical grass pasture soil under Acacia trees in Senegal (Dry season) |
49 |
33 |
0.210 |
0.049 |
33 |
|
Nso_80 |
Tropical grass pasture soil under Acacia trees in Senegal (Rainy season) |
68 |
32 |
-0.495 |
-1.030 |
33 |
|
Nso_81 |
Alpine dry meadow soils in the Colorado Rocky Mountains |
159 |
121 |
-0.747 |
-0.974 |
34 |
|
Nso_86 |
Soil from Kolmberg, an oak-hornbeam forest in the eastern part of Austria |
46 |
41 |
-0.717 |
0.242 |
35 |
|
Nso_87 |
Soil from Rothwald, a spruce-fir-beach forest in the eastern part of Austria |
50 |
41 |
-0.703 |
-0.492 |
35 |
|
Nso_88 |
Soil from Stampfital, an Austrian pine forest in the eastern part of Austria |
41 |
35 |
-0.539 |
-0.877 |
35 |
|
Nso_9 |
Rhizosphere samples from natural grass pasture soils in Scotland |
138 |
118 |
-1.468 |
0.078 |
20 |
|
Nso_96 |
Loamy sand soil from Dunnwald forest in the suburban area of Cologne, Germany (pH 3.9) |
135 |
48 |
-0.362 |
-2.193 |
36 |
|
Nso_l_44 |
Leaf litter from a pine forest in central Java, Indonesia |
87 |
62 |
-0.040 |
0.026 |
37 |
|
Nso_p_23 |
PCB-polluted soil collected near Wittenberg, Germany |
123 |
73 |
-0.632 |
-0.765 |
38 |
|
Nso_p_34 |
PCB-polluted soil collected near Wittenberg, Germany |
173 |
48 |
-0.819 |
-1.018 |
39 |
|
Nso_p_67 |
Heavy metal-contaminated rhizosphere of a metal-hyperaccululating plant and contaminated bulk soil |
282 |
164 |
-2.056 |
-2.229 |
40 |
|
Nsp_1 |
Sediment from Bor Khlueng hot spring in Ratchaburi province, Thailand (50-57C) |
38 |
32 |
0.533 |
0.829 |
41 |
|
Nsp_7 |
Sediment from Obsidian Pool hot spring, Yellowstone National Park U.S.A. (75-95C) |
129 |
53 |
1.113 |
1.342 |
42 |
|
Nsp_93 |
Obsidian Pool Prime hot spring, Yellowstone National Park U.S.A. (74C) - colonized growth slide |
181 |
19 |
0.025 |
-0.826 |
43 |
|
Nsp_94 |
Queen's Laundry hot spring, Yellowstone National Park U.S.A. (89C) - colonized growth slide |
17 |