Widespread diffuse venting and large microbial iron-mounds in the Red Sea

[1]  P. Tapponnier,et al.  Structure and Morphology of the Red Sea. From the Mid-Ocean Ridge to the Ocean-Continent Boundary , 2023, SSRN Electronic Journal.

[2]  C. Mertens,et al.  Volcanically hosted venting with indications of ultramafic influence at Aurora hydrothermal field on Gakkel Ridge , 2022, Nature Communications.

[3]  Peng Zhou,et al.  Metagenomic Features Characterized with Microbial Iron Oxidoreduction and Mineral Interaction in Southwest Indian Ridge , 2022, Microbiology spectrum.

[4]  Xuan Zhang,et al.  Characterization of anaerobic oxidation of methane and microbial community in landfills with aeration. , 2022, Environmental research.

[5]  A. Boyce,et al.  Sulfur isotopes of hydrothermal vent fossils and insights into microbial sulfur cycling within a lower Paleozoic (Ordovician‐early Silurian) vent community , 2022, Geobiology.

[6]  C. Devey,et al.  13 million years of seafloor spreading throughout the Red Sea Basin , 2021, Nature Communications.

[7]  Shawn W. Polson,et al.  Aerobic and anaerobic iron oxidizers together drive denitrification and carbon cycling at marine iron-rich hydrothermal vents , 2020, The ISME Journal.

[8]  Shawn W. Polson,et al.  Validating the Cyc2 Neutrophilic Iron Oxidation Pathway Using Meta-omics of Zetaproteobacteria Iron Mats at Marine Hydrothermal Vents , 2020, mSystems.

[9]  E. Menini,et al.  An atlas of protected hydrothermal vents , 2019, Marine Policy.

[10]  I. Hoteit,et al.  Rapid Red Sea Deep Water renewals caused by volcanic eruptions and the North Atlantic Oscillation , 2018, Science Advances.

[11]  T. Pichler,et al.  Bacterial Diversity and Biogeochemistry of Two Marine Shallow-Water Hydrothermal Systems off Dominica (Lesser Antilles) , 2017, Front. Microbiol..

[12]  K. Haase,et al.  Lower crustal hydrothermal circulation at slow-spreading ridges: evidence from chlorine in Arctic and South Atlantic basalt glasses and melt inclusions , 2017, Contributions to Mineralogy and Petrology.

[13]  H. Dahle,et al.  Environmental controls on biomineralization and Fe-mound formation in a low-temperature hydrothermal system at the Jan Mayen Vent Fields , 2017 .

[14]  C. Moyer,et al.  Hidden diversity revealed by genome-resolved metagenomics of iron-oxidizing microbial mats from Lō’ihi Seamount, Hawai’i , 2017, The ISME Journal.

[15]  Natalia N. Ivanova,et al.  Genome-Based Taxonomic Classification of Bacteroidetes , 2016, Front. Microbiol..

[16]  J. Copley,et al.  Ecology and biogeography of megafauna and macrofauna at the first known deep-sea hydrothermal vents on the ultraslow-spreading Southwest Indian Ridge , 2016, Scientific Reports.

[17]  C. Devey,et al.  Geomorphology of the central Red Sea Rift: Determining spreading processes , 2016 .

[18]  Niklaus J. Grünwald,et al.  Metacoder: An R package for visualization and manipulation of community taxonomic diversity data , 2016, bioRxiv.

[19]  Paul J. McMurdie,et al.  DADA2: High resolution sample inference from Illumina amplicon data , 2016, Nature Methods.

[20]  T. Shibuya,et al.  PIXE and microthermometric analyses of fluid inclusions in hydrothermal quartz from the 2.2Ga Ongeluk Formation, South Africa: Implications for ancient seawater salinity , 2016 .

[21]  R. Toonen,et al.  A review of contemporary patterns of endemism for shallow water reef fauna in the Red Sea , 2016 .

[22]  Sven Petersen,et al.  Hydrothermal exploration of mid-ocean ridges: Where might the largest sulfide deposits be forming? , 2016 .

[23]  T. Hori,et al.  Ecophysiology of Zetaproteobacteria Associated with Shallow Hydrothermal Iron-Oxyhydroxide Deposits in Nagahama Bay of Satsuma Iwo-Jima, Japan , 2016, Front. Microbiol..

[24]  P. Legendre,et al.  Biodiversity patterns, environmental drivers and indicator species on a high-temperature hydrothermal edifice, Mid-Atlantic Ridge , 2015 .

[25]  E. Baker,et al.  Where are the undiscovered hydrothermal vents on oceanic spreading ridges , 2015 .

[26]  C. Devey,et al.  Hydrothermal activity at the ultraslow- to slow-spreading Red Sea Rift traced by chlorine in basalt , 2015 .

[27]  C. Devey,et al.  The rifting to spreading transition in the Red Sea , 2014 .

[28]  M. Hannington,et al.  Early depositional history of metalliferous sediments in the Atlantis II Deep of the Red Sea: Evidence from rare earth element geochemistry , 2014 .

[29]  J. Lloyd,et al.  Biogeochemical implications of the ubiquitous colonization of marine habitats and redox gradients by Marinobacter species , 2013, Front. Microbiol..

[30]  K. Haase,et al.  High mantle temperatures following rifting caused by continental insulation , 2013 .

[31]  Y. Marcon,et al.  Megafaunal distribution and assessment of total methane and sulfide consumption by mussel beds at Menez Gwen hydrothermal vent, based on geo-referenced photomosaics , 2013 .

[32]  Pelin Yilmaz,et al.  The SILVA ribosomal RNA gene database project: improved data processing and web-based tools , 2012, Nucleic Acids Res..

[33]  R. Davis,et al.  Ultra-diffuse hydrothermal venting supports Fe-oxidizing bacteria and massive umber deposition at 5000 m off Hawaii , 2011, The ISME Journal.

[34]  Marcel Martin.  Cutadapt removes adapter sequences from high-throughput sequencing reads , 2011 .

[35]  A. Templeton.  Geomicrobiology of Iron in Extreme Environments , 2011 .

[36]  David Emerson,et al.  Iron-oxidizing bacteria: an environmental and genomic perspective. , 2010, Annual review of microbiology.

[37]  K. Haase,et al.  Diking, young volcanism and diffuse hydrothermal activity on the southern Mid-Atlantic Ridge: The Lilliput field at 9°33'S , 2009 .

[38]  T. Lilburn,et al.  A Novel Lineage of Proteobacteria Involved in Formation of Marine Fe-Oxidizing Microbial Mat Communities , 2007, PloS one.

[39]  D. Lovley,et al.  Extending the Upper Temperature Limit for Life , 2003, Science.

[40]  F. G. Ferris,et al.  Characterization of Bacteriogenic Iron Oxide Deposits from Axial Volcano, Juan de Fuca Ridge, Northeast Pacific Ocean , 2003 .

[41]  C. German,et al.  Evolution and Biogeography of Deep-Sea Vent and Seep Invertebrates , 2002, Science.

[42]  Td Boyd,et al.  Microbial and hydrothermal aspects of ferric oxyhydroxides and ferrosic hydroxides: the example of Franklin Seamount, Western Woodlark Basin, Papua New Guinea , 2001 .

[43]  N. Pace.  A molecular view of microbial diversity and the biosphere. , 1997, Science.

[44]  M. Russell,et al.  The emergence of life from iron monosulphide bubbles at a submarine hydrothermal redox and pH front , 1997, Journal of the Geological Society.

[45]  Y. Fouquet,et al.  Where are the large hydrothermal sulphide deposits in the oceans? , 1997, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.

[46]  A. Isley.  Hydrothermal Plumes and the Delivery of Iron to Banded Iron Formation , 1995, The Journal of Geology.

[47]  E. Bonatti.  Punctiform initiation of seafloor spreading in the Red Sea during transition from a continental to an oceanic rift , 1985, Nature.

[48]  V. S. Yastrebov,et al.  Red sea submersible research expedition , 1982 .

[49]  David L. Williams,et al.  Submarine Thermal Springs on the Gal�pagos Rift , 1979, Science.

[50]  R. G. Pritchard,et al.  A hydrothermal deposit from the floor of the Gulf of Aden , 1977, Mineralogical Magazine.

[51]  F. W. Dickson,et al.  The solubility of anhydrite (CaSO4) in NaCl-H2O from 100 to 450°C and 1 to 1000 bars , 1969 .

[52]  J. Crease,et al.  Hot Salty Water at the Bottom of the Red Sea , 1965, Nature.

[53]  G. Gunter.  Predominance of the Young among Marine Fishes Found in Fresh Water , 1957 .

[54]  F. Robert,et al.  Warm Archean oceans reconstructed from oxygen isotope composition of early-life remnants , 2017 .

[55]  F. Sirocko.  Global change: Ups and downs in the Red Sea , 2003, Nature.

[56]  B. Sichler,et al.  Tectonics of the westernmost Gulf of Aden and the Gulf of Tadjoura from submersible observations , 1986, Nature.