# | Title | Journal | Year | Citations |
---|
1 | Exopolymeric substances of sulfate‐reducing bacteria: Interactions with calcium at alkaline pH and implication for formation of carbonate minerals | Geobiology | 2007 | 492 |
2 | Serpentinization as a source of energy at the origin of life | Geobiology | 2010 | 411 |
3 | Towards a consistent classification scheme for geochemical environments, or, why we wish the term ‘suboxic’ would go away | Geobiology | 2009 | 324 |
4 | Geological and trace element evidence for a marine sedimentary environment of deposition and biogenicity of 3.45 Ga stromatolitic carbonates in the Pilbara Craton, and support for a reducing Archaean ocean | Geobiology | 2003 | 295 |
5 | A coupled atmosphere-ecosystem model of the early Archean Earth | Geobiology | 2005 | 281 |
6 | Cyanobacterial calcification, carbon dioxide concentrating mechanisms, and Proterozoic?Cambrian changes in atmospheric composition | Geobiology | 2006 | 266 |
7 | Biological weathering and the long‐term carbon cycle: integrating mycorrhizal evolution and function into the current paradigm | Geobiology | 2009 | 263 |
8 | Microbial fuel cell energy from an ocean cold seep | Geobiology | 2006 | 255 |
9 | Oxygen, animals and oceanic ventilation: an alternative view | Geobiology | 2009 | 255 |
10 | Sulphate-reducing bacteria induce low-temperature Ca-dolomite and high Mg-calcite formation | Geobiology | 2003 | 253 |
11 | Fe(III) mineral formation and cell encrustation by the nitrate-dependent Fe(II)-oxidizer strain BoFeN1 | Geobiology | 2005 | 250 |
12 | The loss of mass-independent fractionation in sulfur due to a Palaeoproterozoic collapse of atmospheric methane | Geobiology | 2006 | 246 |
13 | Oceanic oxygenation events in the anoxic Ediacaran ocean | Geobiology | 2016 | 241 |
14 | Multiple sulphur isotopic interpretations of biosynthetic pathways: implications for biological signatures in the sulphur isotope record | Geobiology | 2003 | 234 |
15 | Extracellular electron transfer: wires, capacitors, iron lungs, and more | Geobiology | 2008 | 232 |
16 | Timing of morphological and ecological innovations in the cyanobacteria – a key to understanding the rise in atmospheric oxygen | Geobiology | 2010 | 228 |
17 | The mechanisms of iron isotope fractionation produced during dissimilatory Fe(III) reduction by Shewanella putrefaciens and Geobacter sulfurreducens | Geobiology | 2007 | 224 |
18 | Abiotic oxidation of Fe(II) by reactive nitrogen species in cultures of the nitrate‐reducing Fe(II) oxidizer Acidovorax sp. BoFeN1 – questioning the existence of enzymatic Fe(II) oxidation | Geobiology | 2013 | 224 |
19 | TEM evidence for eukaryotic diversity in mid-Proterozoic oceans | Geobiology | 2004 | 219 |
20 | The potential significance of microbial Fe(III) reduction during deposition of Precambrian banded iron formations | Geobiology | 2005 | 212 |
21 | Archaeal and bacterial communities in geochemically diverse hot springs of Yellowstone National Park, USA | Geobiology | 2005 | 203 |
22 | Cyanobacterial calcification and its rock-building potential during 3.5 billion years of Earth history | Geobiology | 2006 | 196 |
23 | Biological energy requirements as quantitative boundary conditions for life in the subsurface | Geobiology | 2004 | 186 |
24 | Microbialites and global environmental change across the Permian–Triassic boundary: a synthesis | Geobiology | 2012 | 184 |
25 | An inorganic geochemical argument for coupled anaerobic oxidation of methane and iron reduction in marine sediments | Geobiology | 2014 | 180 |
26 | Climate and vegetational regime shifts in the late Paleozoic ice age earth | Geobiology | 2009 | 178 |
27 | Palaeozoic tropical rainforests and their effect on global climates: is the past the key to the present? | Geobiology | 2005 | 176 |
28 | The control of organic matter on microbially mediated iron reduction and arsenic release in shallow alluvial aquifers, Cambodia | Geobiology | 2007 | 176 |
29 | Recent ecological and biogeochemical changes in alpine lakes of Rocky Mountain National Park (Colorado, USA): a response to anthropogenic nitrogen deposition | Geobiology | 2003 | 175 |
30 | Molecular characterization of microbial communities in deep coal seam groundwater of northern Japan | Geobiology | 2007 | 171 |
31 | Sterols in red and green algae: quantification, phylogeny, and relevance for the interpretation of geologic steranes | Geobiology | 2008 | 168 |
32 | Scanning transmission X-ray microscopy study of microbial calcification | Geobiology | 2004 | 166 |
33 | Bacterial, archaeal and eukaryotic diversity of smooth and pustular microbial mat communities in the hypersaline lagoon of Shark Bay | Geobiology | 2009 | 164 |
34 | Reshaping of sandstone surfaces by cryptoendolithic cyanobacteria: bioalkalization causes chemical weathering in arid landscapes | Geobiology | 2004 | 160 |
35 | The methane cycle in ferruginous Lake Matano | Geobiology | 2011 | 159 |
36 | Biogeochemical modelling of the rise in atmospheric oxygen | Geobiology | 2006 | 156 |
37 | The geological consequences of evolution | Geobiology | 2003 | 154 |
38 | Where's the glass? Biomarkers, molecular clocks, and microRNAs suggest a 200‐Myr missing Precambrian fossil record of siliceous sponge spicules | Geobiology | 2010 | 154 |
39 | Crown group Oxyphotobacteria postdate the rise of oxygen | Geobiology | 2017 | 153 |
40 | Diversity of ammonia monooxygenase (amoA) genes across environmental gradients in Chesapeake Bay sediments | Geobiology | 2003 | 149 |
41 | A high‐resolution chemical and structural study of framboidal pyrite formed within a low‐temperature bacterial biofilm | Geobiology | 2008 | 143 |
42 | Microbial colonization of Ca-sulfate crusts in the hyperarid core of the Atacama Desert: implications for the search for life on Mars | Geobiology | 2011 | 143 |
43 | Growth of synthetic stromatolites and wrinkle structures in the absence of microbes – implications for the early fossil record | Geobiology | 2008 | 141 |
44 | Coevolution of metal availability and nitrogen assimilation in cyanobacteria and algae | Geobiology | 2009 | 141 |
45 | Precipitation of low‐temperature dolomite from an anaerobic microbial consortium: the role of methanogenic Archaea | Geobiology | 2009 | 141 |
46 | A late methanogen origin for molybdenum‐dependent nitrogenase | Geobiology | 2011 | 141 |
47 | Inside the alkalinity engine: the role of electron donors in the organomineralization potential of sulfate‐reducing bacteria | Geobiology | 2012 | 139 |
48 | Biostabilization of cohesive sediments: revisiting the role of abiotic conditions, physiology and diversity of microbes, polymeric secretion, and biofilm architecture | Geobiology | 2015 | 136 |
49 | Patterns of sulfur isotope fractionation during microbial sulfate reduction | Geobiology | 2016 | 136 |
50 | Morphological and habitat evolution in the Cyanobacteria using a compartmentalization approach | Geobiology | 2005 | 134 |