Candidatus Scalindua: Difference between revisions

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"'''''[[Candidatus]]''''' '''Scalindua'''" is a [[bacterial]] [[genus]], member of the order [[Planctomycetes]].<ref name="SchmidWalsh2003">{{cite journal|last1=Schmid|first1=Markus|last2=Walsh|first2=Kerry|last3=Webb|first3=Rick|last4=Rijpstra|first4=W. Irene|last5=van de Pas-Schoonen|first5=Katinka|last6=Verbruggen|first6=Mark Jan|last7=Hill|first7=Thomas|last8=Moffett|first8=Bruce|last9=Fuerst|first9=John|last10=Schouten|first10=Stefan|last11=Sinninghe Damsté|first11=Jaap S.|last12=Harris|first12=James|last13=Shaw|first13=Phil|last14=Jetten|first14=Mike|last15=Strous|first15=Marc|title=Candidatus "Scalindua brodae", sp. nov., Candidatus "Scalindua wagneri", sp. nov., Two New Species of Anaerobic Ammonium Oxidizing Bacteria|journal=Systematic and Applied Microbiology|volume=26|issue=4|year=2003|pages=529–538|issn=0723-2020|doi=10.1078/072320203770865837|pmid=14666981}}</ref> These bacteria lack [[peptidoglycan]] in its [[cell wall]] and have a compartmentalized [[cytoplasm]]. They are [[ammonium]] oxidising bacteria found in marine environments.
"'''''[[Candidatus]]''''' '''Scalindua'''" is a [[bacterial]] [[genus]], member of the order [[Planctomycetes]].<ref name="SchmidWalsh2003">{{cite journal|last1=Schmid|first1=Markus|last2=Walsh|first2=Kerry|last3=Webb|first3=Rick|last4=Rijpstra|first4=W. Irene|last5=van de Pas-Schoonen|first5=Katinka|last6=Verbruggen|first6=Mark Jan|last7=Hill|first7=Thomas|last8=Moffett|first8=Bruce|last9=Fuerst|first9=John|last10=Schouten|first10=Stefan|last11=Sinninghe Damsté|first11=Jaap S.|last12=Harris|first12=James|last13=Shaw|first13=Phil|last14=Jetten|first14=Mike|last15=Strous|first15=Marc|title=Candidatus "Scalindua brodae", sp. nov., Candidatus "Scalindua wagneri", sp. nov., Two New Species of Anaerobic Ammonium Oxidizing Bacteria|journal=Systematic and Applied Microbiology|volume=26|issue=4|year=2003|pages=529–538|issn=0723-2020|doi=10.1078/072320203770865837|pmid=14666981}}</ref> These bacteria lack [[peptidoglycan]] in its [[cell wall]] and have a compartmentalized [[cytoplasm]]. They are [[ammonium]] oxidising bacteria found in marine environments.

== Introduction ==
"'''''[[Candidatus]]''''' '''Scalindua'''" is a [[bacterial]] [[genus]], member of the order [[Planctomycetes]]. These bacteria lack [[peptidoglycan]] in its [[cell wall]] and have a compartmentalized [[cytoplasm]]. <ref name=":7" />. Candidatus Scalindua can be further divided into three species: Scalindua brodae, Scalindua wagneri, and Scalindua sorokinii. They are [[ammonium]] oxidising bacteria found in marine environments. The genus Scalindua are the most abundant annamox bacteria in marine environments, so they are extremely vital in the Earth's nitrogen cycle.<ref name=":7" />

== Metabolism ==
Scalindua are [[Anaerobic organism|anaerobic]] [[anammox]] (ammonium oxidizing) bacteria<ref name=":6">{{Cite journal|last=Awata|first=Takanori|last2=Oshiki|first2=Mamoru|last3=Kindaichi|first3=Tomonori|last4=Ozaki|first4=Noriatsu|last5=Ohashi|first5=Akiyoshi|last6=Okabe|first6=Satoshi|date=2017-03-08|title=Physiological Characterization of an Anaerobic Ammonium-Oxidizing Bacterium Belonging to the “Candidatus Scalindua” Group|url=http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3697556/|journal=Applied and Environmental Microbiology|volume=79|issue=13|pages=4145–4148|doi=10.1128/AEM.00056-13|issn=0099-2240|pmc=PMC3697556|pmid=23584767}}</ref>. The ammonium-oxidizing reaction composes a significant part of the global [[nitrogen cycle]], by some estimates it is the cause of up to 50% of total nitrogen turnover in marine environments<ref>{{Cite journal|last=Kuenen|first=J. Gijs|date=2008-04-01|title=Anammox bacteria: from discovery to application|url=http://www.nature.com/nrmicro/journal/v6/n4/full/nrmicro1857.html|journal=Nature Reviews Microbiology|language=en|volume=6|issue=4|pages=320–326|doi=10.1038/nrmicro1857|issn=1740-1526}}</ref>. It consists of the oxidization of ammonium using nitrite as an electron acceptor (both are fixed nitrogen) and subsequent generation of nitrogen gas:

“NH4+ + NO2- = N2 + 2H2O (ΔG° = -357 kj mol-1)”<ref name=":5">{{Cite web|url=https://microbewiki.kenyon.edu/index.php/Anammox#References|title=Anammox Bacteria|last=|first=|date=|website=Microbewiki|archive-url=|archive-date=|dead-url=|access-date=}}</ref>

This reaction uses nitrite (NO2-) as a terminal electron acceptor to produce nitric oxide (NO), which is then combined with ammonium (NH4+) to produce the intermediate [[hydrazine]] (N2H4) and water (H2O). [[Hydrazine]], a very reactive molecule also used for rocket fuel, is then oxidized into nitrogen gas (N2)<ref>{{Cite book|url=https://www.worldcat.org/oclc/797831085|title=Advances in microbial physiology Volume 60|last=K.|first=Poole, Robert|date=2012-01-01|publisher=Elsevier/Academic Press|isbn=9780123982643|oclc=797831085}}</ref>. The half reactions may be represented as:

“NO2- + 2H+ + e- = NO + H2O (E° = +0.38V)

NO + NH4+ + 2H+ + 3e- = N2H4 + H2O (E° = +0.06V)
[[File:Anammox mechanism 1.png|thumb|308x308px|Mechanism of Ammonium Oxidation]]
N2H4 = N2 + 4H+ + 4e- (E° = -0.75V)”<ref name=":5" />

This metabolic pathway occurs anaerobically, something that was once considered impossible as ammonium was thought to be inert in the absence of oxygen<ref>{{Cite web|url=http://www.annualreviews.org/doi/10.1146/annurev.micro.58.030603.123605|title=Anaerobic Oxidation of Methane and Ammonium|last=Strous|first=Marc|last2=Jetten|first2=Mike S. M.|date=2004-09-13|website=http://dx.doi.org/10.1146/annurev.micro.58.030603.123605|language=en|doi=10.1146/annurev.micro.58.030603.123605|access-date=2017-03-08}}</ref>. In fact, the presence of oxygen over 2 uM inhibits the anammox pathway, which is why Scalindua respire anaerobically<ref name=":5" />.

These reactions occur in a large membrane-bound cellular organelle called the anammoxosome, which contains an electron transport chain and an ATPase that pumps protons back into the cytoplasm from the anammoxosome lumen. It functions much like a mitochondrion in eukaryotic cells. The anammoxosome membrane is invaginated (folded in upon itself) to increase its surface area<ref>{{Cite journal|last=Niftrik|first=Laura van|last2=Jetten|first2=Mike S. M.|date=2012-09-01|title=Anaerobic Ammonium-Oxidizing Bacteria: Unique Microorganisms with Exceptional Properties|url=http://mmbr.asm.org/content/76/3/585|journal=Microbiology and Molecular Biology Reviews|language=en|volume=76|issue=3|pages=585–596|doi=10.1128/MMBR.05025-11|issn=1092-2172|pmc=PMC3429623|pmid=22933561}}</ref>. The existence of membrane-bound cellular organelles is very unusual in prokaryotes, and appears to be limited to the [[planctomycetes]] phylum<ref>{{Cite journal|last=Kuenen|first=J. Gijs|date=2008-04-01|title=Anammox bacteria: from discovery to application|url=http://www.nature.com/nrmicro/journal/v6/n4/full/nrmicro1857.html|journal=Nature Reviews Microbiology|language=en|volume=6|issue=4|pages=320–326|doi=10.1038/nrmicro1857|issn=1740-1526}}</ref>.

Scalindua and other anammox bacteria fix carbon using carbon dioxide as a carbon source. Metagenomic analysis has revealed the presence of genes responsible for the “[[reductive acetyl-CoA pathway]] (also known as the [[Wood–Ljungdahl pathway|Wood-Ljungdahl pathway]]) which allows for the creation of the precursor molecule [[Acetyl-CoA|acetyl CoA]] from carbon dioxide<ref name=":10">{{Cite journal|last=van de Vossenberg|first=Jack|last2=Woebken|first2=Dagmar|last3=Maalcke|first3=Wouter J|last4=Wessels|first4=Hans J C T|last5=Dutilh|first5=Bas E|last6=Kartal|first6=Boran|last7=Janssen-Megens|first7=Eva M|last8=Roeselers|first8=Guus|last9=Yan|first9=Jia|date=2017-03-08|title=The metagenome of the marine anammox bacterium ‘Candidatus Scalindua profunda’ illustrates the versatility of this globally important nitrogen cycle bacterium|url=http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3655542/|journal=Environmental Microbiology|volume=15|issue=5|pages=1275–1289|doi=10.1111/j.1462-2920.2012.02774.x|issn=1462-2912|pmc=PMC3655542|pmid=22568606}}</ref><ref>{{Cite journal|last=Kartal|first=Boran|last2=Almeida|first2=De|last3=M|first3=Naomi|last4=Maalcke|first4=Wouter J.|last5=Camp|first5=Op den|last6=J.m|first6=Huub|last7=Jetten|first7=Mike S. M.|last8=Keltjens|first8=Jan T.|date=2013-05-01|title=How to make a living from anaerobic ammonium oxidation|url=https://academic.oup.com/femsre/article/37/3/428/585200/How-to-make-a-living-from-anaerobic-ammonium|journal=FEMS Microbiology Reviews|volume=37|issue=3|pages=428–461|doi=10.1111/1574-6976.12014|issn=0168-6445}}</ref>.  
== Discovery and Distribution ==
[[Ammonium]] and [[methane]] are known to be relatively difficult to activate with reactions catalyzed by enzymes that make use of high-potential [[oxygen radicals]], which are unavailable to [[anaerobic]] life leading to the assumption that both compounds where effectively inactive in low oxygen environments<ref name=":0">{{Cite web|url=http://www.annualreviews.org/doi/10.1146/annurev.micro.58.030603.123605|title=Anaerobic Oxidation of Methane and Ammonium|last=Strous|first=Marc|last2=Jetten|first2=Mike S. M.|date=2004-09-13|website=http://dx.doi.org/10.1146/annurev.micro.58.030603.123605|language=en|doi=10.1146/annurev.micro.58.030603.123605|access-date=2017-03-07}}</ref>. Throughout the 1970s and 80s, results from several independent studies exploring relationships between methane and [[sulfate]] concentrations in marine sediments found indication that anaerobic methane [[Redox|oxidation]] was in fact a widespread occurrence<ref name=":0" />. It was not until 1999 that the existence of aerobic ammonium oxidation was first discovered in a wastewater treatment plant in The Netherlands and given the name “[[anammox]],” which would later prove to be a key player as part of the marine [[nitrogen cycle]]<ref name=":0" /><ref name=":1">{{Cite journal|last=Jetten|first=Mike S. M.|last2=Strous|first2=Marc|last3=Fuerst|first3=John A.|last4=Kramer|first4=Evelien H. M.|last5=Logemann|first5=Susanne|last6=Muyzer|first6=Gerard|last7=Pas-Schoonen|first7=Katinka T. van de|last8=Webb|first8=Richard|last9=Kuenen|first9=J. Gijs|title=http://www.nature.com/doifinder/10.1038/22749|url=http://www.nature.com/doifinder/10.1038/22749|journal=Nature|volume=400|issue=6743|pages=446–449|doi=10.1038/22749}}</ref><ref name=":2">{{Cite journal|last=Dalsgaard|first=Tage|last2=Canfield|first2=Donald E.|last3=Petersen|first3=Jan|last4=Thamdrup|first4=Bo|last5=Acuña-González|first5=Jenaro|title=N2 production by the anammox reaction in the anoxic water column of Golfo Dulce, Costa Rica|url=http://www.nature.com/doifinder/10.1038/nature01526|journal=Nature|volume=422|issue=6932|pages=606–608|doi=10.1038/nature01526}}</ref>. Some known anammox bacteria include Candidatus Scalindua, Kuenenia, [[Brocadia anammoxidans|Brocadia]], Jettenia and Anammoxoglobus<ref name=":3">{{Cite journal|last=Woebken|first=Dagmar|last2=Lam|first2=Phyllis|last3=Kuypers|first3=Marcel M. M.|last4=Naqvi|first4=S. Wajih A.|last5=Kartal|first5=Boran|last6=Strous|first6=Marc|last7=Jetten|first7=Mike S. M.|last8=Fuchs|first8=Bernhard M.|last9=Amann|first9=Rudolf|date=2008-11-01|title=A microdiversity study of anammox bacteria reveals a novel Candidatus Scalindua phylotype in marine oxygen minimum zones|url=http://onlinelibrary.wiley.com/doi/10.1111/j.1462-2920.2008.01640.x/abstract|journal=Environmental Microbiology|language=en|volume=10|issue=11|pages=3106–3119|doi=10.1111/j.1462-2920.2008.01640.x|issn=1462-2920}}</ref>. Of these bacteria, only Candidatus Scalindua spp. can be found in marine ecosystems<ref name=":3" />.

During the past, many microorganisms such as anammox bacteria may have escaped discovery due to their relatively low growth rate requiring very efficient biomass retention absent from classical methods of cultivation<ref name=":4">{{Cite journal|last=Strous|first=M.|last2=Heijnen|first2=J. J.|last3=Kuenen|first3=J. G.|last4=Jetten|first4=M. S. M.|date=1998-11-01|title=The sequencing batch reactor as a powerful tool for the study of slowly growing anaerobic ammonium-oxidizing microorganisms|url=https://link.springer.com/article/10.1007/s002530051340|journal=Applied Microbiology and Biotechnology|language=en|volume=50|issue=5|pages=589–596|doi=10.1007/s002530051340|issn=0175-7598}}</ref>. With the use of [[Biofilm|biofilms]] to improve the culturability of organisms that naturally occur in biofilms in combination with the use of biomass retention to study slowly growing microorganisms under substrate limitation, a technique using [[Sequencing batch reactor|sequencing batch reactors]] (SBR) was developed for the long-term enrichment, cultivation, and quantitative analysis of a very slowly growing microbial community<ref name=":4" />. Phylogenetic analysis of the first anamox bacteria discovered concluded that the organisms branched deeply into the [[Planctomycetes]] phylum, which was previously considered to be of limited environmental importance<ref name=":1" />. Nitrogen loses that could only be explained by the process of anammox continued to be discovered in freshwater waste treatment facilities around the world including North America, Asia, and multiple regions throughout Europe<ref>{{Cite journal|last=Schmid|first=Markus C.|last2=Maas|first2=Bart|last3=Dapena|first3=Ana|last4=Pas-Schoonen|first4=Katinka van de|last5=Vossenberg|first5=Jack van de|last6=Kartal|first6=Boran|last7=Niftrik|first7=Laura van|last8=Schmidt|first8=Ingo|last9=Cirpus|first9=Irina|date=2005-04-01|title=Biomarkers for In Situ Detection of Anaerobic Ammonium-Oxidizing (Anammox) Bacteria|url=http://aem.asm.org/content/71/4/1677|journal=Applied and Environmental Microbiology|language=en|volume=71|issue=4|pages=1677–1684|doi=10.1128/AEM.71.4.1677-1684.2005|issn=0099-2240|pmc=PMC1082507|pmid=15811989}}</ref>. Scalindua’s role in the marine nitrogen cycle has been found to be of importance regarding the reduction of nitrate to atmospheric nitrogen in the anoxic regions of the ocean<ref name=":2" />. Since primary productivity in the ocean is often limited by nitrogen availability, the removal of usable nitrogen in sediments through anammox by Scalindua may significantly affect [[Biogeochemical cycle|biogeochemical cycles]] in anoxic waters<ref name=":2" />. In certain regions, such as the [[Golfo Dulce, Costa Rica|Golfo Dulce]] in Costa Rica, up to %35 of atmospheric nitrogen production in the water column can be attributed to Scalindua spp<ref name=":2" />. In other regions such as the [[Black Sea]], the worlds largest anoxic basin characterized by a large gradient in ammonium concentrations (high levels in deep water tapering off to only trace amounts in the suboxic zone), the apparent ammonium sink in the suboxic zone was identified to be the result of anaerobic oxidation by Scalindua spp<ref>{{Cite journal|last=Kuypers|first=Marcel M. M.|last2=Sliekers|first2=A. Olav|last3=Lavik|first3=Gaute|last4=Schmid|first4=Markus|last5=Jørgensen|first5=Bo Barker|last6=Kuenen|first6=J. Gijs|last7=Damsté|first7=Jaap S. Sinninghe|last8=Strous|first8=Marc|last9=Jetten|first9=Mike S. M.|title=Anaerobic ammonium oxidation by anammox bacteria in the Black Sea|url=http://www.nature.com/doifinder/10.1038/nature01472|journal=Nature|volume=422|issue=6932|pages=608–611|doi=10.1038/nature01472}}</ref>.

== Morphology ==
Organisms within the genus “Candidatus Scalindua” are classified as [[Gram-negative bacteria|gram-negative]] chemolithoautotrophic bacteria <ref name=":6">{{Cite journal|last=Strous|first=M.|year=1999|title=Missing lithotroph identified as new planctomycete|url=|journal=Nature|volume=400 [6743]|pages=446-449|via=}}</ref>. This means that their carbon and energy largely come from inorganic sources. Furthermore, Scalindua are obligate anaerobes, so they are unable live in oxygen-rich environments <ref name=":6" /><ref name=":7">{{Cite journal|last=Schmid|first=Markus|year=2003|title=Candidatus “Scalindua brodae”, sp. nov., Candidatus “Scalindua wagneri”, sp. nov., Two New Species of Anaerobic Ammonium Oxidizing Bacteria|url=|journal=Systematic and Applied Microbiology|volume=26 [4]|pages=529-538|via=}}</ref>.

 As with all other organisms within the order [[Planctomycetes]], the cell wall of these organisms does not contain [[peptidoglycan]]<ref name=":7" /><ref>{{Cite journal|last=Lindsay|first=M.R,|year=2001|title=Cell compartmentalisation in planctomycetes: novel types of structural organisation for the bacterial cell.|url=|journal=Archives of Microbiology|volume=175 [6]|pages=413-429|via=}}</ref>. Scalindua are spherical in shape, with a diameter of roughly one micrometer, and contain compartmentalized cytoplasms<ref name=":7" />. Furthermore, organisms within Candidatus Scalindua have two inner membranes instead of one inner, and one outer surrounding the cell wall.<ref>{{Cite journal|last=van Niftrick|first=Laura A.|year=2004|title=The anammoxosome: an intracytoplasmic compartment in anammox bacteria|url=|journal=FEMS Microbiology Letters|volume=233 (1)|pages=7-13|via=}}</ref> Cells within Scalindua wagenri are oriented into compact clusters, whereas Scalindua brodae’s cells are found to be more loosely packed<ref name=":7" />. All Scalindua contain unique organelles called Anammoxosomes, which are membrane bound within the cytoplasm<ref name=":7" /><ref name=":8">{{Cite journal|last=Sinninghe|first=Damste|year=2002|title=Linearly concatenated cyclobutane lipids form a dense bacterial membrane|url=|journal=Nature|volume=419|pages=708-712|via=}}</ref>. Anammoxosomes are where the anaerobic ammonium oxidation process occurs. The membrane that surrounds anammoxosomes in [[anammox]] bacteria contain unique lipids called “[[ladderane]]” lipids, which contain a series of cyclobutane ring structures<ref name=":8" />. However, all other membranes within [[anammox]] bacteria are similar to organisms within the order [[Planctomycetes]].

== Evolutionary History ==
According to Strous et. al., [[anammox]]-capability is the result of a singular evolutionary event. All [[anammox]] bacteria are descendents of the same ancient [[planctomycetes]] species that first evolved the [[anammox]] reaction<ref>{{Cite web|url=http://www.annualreviews.org/doi/10.1146/annurev.micro.58.030603.123605|title=Anaerobic Oxidation of Methane and Ammonium|last=Strous|first=Marc|last2=Jetten|first2=Mike S. M.|date=2004-09-13|website=http://dx.doi.org/10.1146/annurev.micro.58.030603.123605|language=en|doi=10.1146/annurev.micro.58.030603.123605|access-date=2017-03-08}}</ref>. The Scalindua genus is the most widespread of all the anammox bacteria genera described so far<ref>{{Cite journal|last=Schmid|first=Markus|last2=Walsh|first2=Kerry|last3=Webb|first3=Rick|last4=Rijpstra|first4=W. Irene C.|last5=van de Pas-Schoonen|first5=Katinka|last6=Verbruggen|first6=Mark Jan|last7=Hill|first7=Thomas|last8=Moffett|first8=Bruce|last9=Fuerst|first9=John|date=2003-11-01|title=Candidatus "Scalindua brodae", sp. nov., Candidatus "Scalindua wagneri", sp. nov., two new species of anaerobic ammonium oxidizing bacteria|url=https://www.ncbi.nlm.nih.gov/pubmed/14666981|journal=Systematic and Applied Microbiology|volume=26|issue=4|pages=529–538|issn=0723-2020|pmid=14666981}}</ref>.

Currently, all [[anammox]] bacteria are thought to be members of the order Brocadiales<ref>{{Cite journal|last=Speth|first=Daan R.|last2=Russ|first2=Lina|last3=Kartal|first3=Boran|last4=op den Camp|first4=Huub J. M.|last5=Dutilh|first5=Bas E.|last6=Jetten|first6=Mike S. M.|date=2015-01-08|title=Draft Genome Sequence of Anammox Bacterium “Candidatus Scalindua brodae,” Obtained Using Differential Coverage Binning of Sequencing Data from Two Reactor Enrichments|url=http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4290996/|journal=Genome Announcements|volume=3|issue=1|doi=10.1128/genomeA.01415-14|issn=2169-8287|pmc=PMC4290996|pmid=25573945}}</ref>.

== Ecological Role ==
''Candidatus'' Scalindua sp. were the only [[Candidatus]] species found in the Black Sea, the Benguela OMZ off the coast of Namibia, and the estuary in the Randers Fjord, Denmark. <ref name=":9">{{Cite journal|last=Schmid|first=Markus C.|last2=Risgaard-Petersen|first2=Nils|last3=Van De Vossenberg|first3=Jack|last4=Kuypers|first4=Marcel M. M.|last5=Lavik|first5=Gaute|last6=Petersen|first6=Jan|last7=Hulth|first7=Stefan|last8=Thamdrup|first8=Bo|last9=Canfield|first9=Don|date=2007-06-01|title=Anaerobic ammonium-oxidizing bacteria in marine environments: widespread occurrence but low diversity|url=http://onlinelibrary.wiley.com/doi/10.1111/j.1462-2920.2007.01266.x/abstract|journal=Environmental Microbiology|language=en|volume=9|issue=6|pages=1476–1484|doi=10.1111/j.1462-2920.2007.01266.x|issn=1462-2920}}</ref> Globally, ''Candidatus'' Scalindua has been discovered in all of the marine environments that have been studied; other marine bacteria are not this ubiquitous.<ref name=":9" /><ref name=":3" />

The ideal environmental conditions, with regards to temperature, pH and salinity for “''Candidatus'' Scalindua sp.” are: 10 to 30°C, 6.0 to 8.5 pH and 0.8% to 4.0% salinity with no activity when salinity was 0%, respectively. <ref>{{Cite journal|last=Awata|first=Takanori|last2=Oshiki|first2=Mamoru|last3=Kindaichi|first3=Tomonori|last4=Ozaki|first4=Noriatsu|last5=Ohashi|first5=Akiyoshi|last6=Okabe|first6=Satoshi|date=2013-07-01|title=Physiological Characterization of an Anaerobic Ammonium-Oxidizing Bacterium Belonging to the “Candidatus Scalindua” Group|url=http://aem.asm.org/content/79/13/4145|journal=Applied and Environmental Microbiology|language=en|volume=79|issue=13|pages=4145–4148|doi=10.1128/AEM.00056-13|issn=0099-2240|pmc=PMC3697556|pmid=23584767}}</ref>

Marine sediments located in deep-sea methane seeps contain [[anammox]] bacteria associated with the ''Candidatus'' Scalindua sp; these bacteria likely have a substantial role in the nitrogen cycle found in the sediments.<ref>{{Cite journal|last=Shao|first=Sudong|last2=Luan|first2=Xiwu|last3=Dang|first3=Hongyue|last4=Zhou|first4=Haixia|last5=Zhao|first5=Yakun|last6=Liu|first6=Haitao|last7=Zhang|first7=Yunbo|last8=Dai|first8=Lingqing|last9=Ye|first9=Ying|date=2014-02-01|title=Deep-sea methane seep sediments in the Okhotsk Sea sustain diverse and abundant anammox bacteria|url=https://academic.oup.com/femsec/article-lookup/doi/10.1111/1574-6941.12241|journal=FEMS Microbiology Ecology|language=en|volume=87|issue=2|pages=503–516|doi=10.1111/1574-6941.12241|issn=0168-6496}}</ref>

Two types of [[anammox]] bacteria, Scalindua (59% abundance) and Kuenenia (41% abundance), have been found in the non-[[rhizosphere]] area of the saltmarsh grass ''Spartina alterniflora'' while only Scalindua was present within the [[rhizosphere]] and at 1.5 times greater than the amount of [[anammox]] bacterial in the non-[[rhizosphere]] sediments.<ref name=":11">{{Cite journal|last=Zheng|first=Yanling|last2=Hou|first2=Lijun|last3=Liu|first3=Min|last4=Yin|first4=Guoyu|last5=Gao|first5=Juan|last6=Jiang|first6=Xiaofen|last7=Lin|first7=Xianbiao|last8=Li|first8=Xiaofei|last9=Yu|first9=Chendi|date=2016-09-01|title=Community composition and activity of anaerobic ammonium oxidation bacteria in the rhizosphere of salt-marsh grass Spartina alterniflora|url=https://link.springer.com/article/10.1007/s00253-016-7625-2|journal=Applied Microbiology and Biotechnology|language=en|volume=100|issue=18|pages=8203–8212|doi=10.1007/s00253-016-7625-2|issn=0175-7598}}</ref> Changing seasons do not affect the make-up of the [[anammox]] bacterial communities within the sediments in and around the [[rhizosphere]]; however there was always a greater abundance of the [[anammox]] bacteria within the [[rhizosphere]], which peaks during July and October when temperature are warmest.<ref name=":11" /> During the warmer parts of the year both communities of the [[anammox]] bacteria within and outside of the rhizosphere are more active and produce more N<sub>2</sub> with the bacteria in the [[rhizosphere]] producing almost twice as much N<sub>2</sub>.<ref name=":11" />

== Taxonomy ==
Candidatus Scalindua is closely related genetically to the other [[Anammox]] bacteria within the order [[Planctomycetes]], such as Candidatus Brocadia and Candidatus Kuenenia.<ref name=":7" />. Yet, Scalindua is quite different from other genuses of [[Anammox]] bacteria on the 16s rRNA level <ref name=":7" />. For example, Candidatus Scalindua and Candidatus Brocadia only share 85% similar sequences <ref name=":7" />. Candidatus Scalindua can be further divided into three species: Scalindua brodae, Scalindua wagneri, and Scalindua sorokinii <ref name=":7" /><ref>{{Cite journal|last=Kuypers|first=M.|year=2003|title=Anaerobic ammonium oxidation by Anammox bacteria in the Black Sea|url=|journal=Nature|volume=422|pages=608-611|via=}}</ref>. Scalindua is the most abundant genus of [[Anammox]] bacteria known to date, making it very important in the world’s aquatic environments. 

== Applications ==
[[Scalindua wagneri]] are often used in wastewater treatment plants as a buffer of sorts to reduce the adverse effects of nitrification and denitrification on the local environment

<ref>{{Cite journal|last=Jetten|first=Mike|year=2004|title="Biodiversity and application of anaerobic ammonium-oxidizing bacteria"|url=|journal=European Symposium on Environmental Biotechnology|volume=|pages=21-26|via=}}</ref>.The use of annamox bacteria in wastewater treatment plants has a drastically reduced cost compared to previous dinitrification methods. Furthermore, it is a much more environmentally friendly method. <ref name=":10" />

== References ==


==Species==
==Species==

Revision as of 07:07, 5 April 2017

Scalindua
Scientific classification
Domain:
Phylum:
Class:
Order:
Family:
Genus:
Scalindua
Binomial name
Candidatus Scalindua
Schmid et al. 2003
Species

Scalindua brodae
Scalindua profunda
Scalindua wagneri

"Candidatus Scalindua" is a bacterial genus, member of the order Planctomycetes.[1] These bacteria lack peptidoglycan in its cell wall and have a compartmentalized cytoplasm. They are ammonium oxidising bacteria found in marine environments.

Introduction

"Candidatus Scalindua" is a bacterial genus, member of the order Planctomycetes. These bacteria lack peptidoglycan in its cell wall and have a compartmentalized cytoplasm. [2]. Candidatus Scalindua can be further divided into three species: Scalindua brodae, Scalindua wagneri, and Scalindua sorokinii. They are ammonium oxidising bacteria found in marine environments. The genus Scalindua are the most abundant annamox bacteria in marine environments, so they are extremely vital in the Earth's nitrogen cycle.[2]

Metabolism

Scalindua are anaerobic anammox (ammonium oxidizing) bacteria[3]. The ammonium-oxidizing reaction composes a significant part of the global nitrogen cycle, by some estimates it is the cause of up to 50% of total nitrogen turnover in marine environments[4]. It consists of the oxidization of ammonium using nitrite as an electron acceptor (both are fixed nitrogen) and subsequent generation of nitrogen gas:

“NH4+ + NO2- = N2 + 2H2O (ΔG° = -357 kj mol-1)”[5]

This reaction uses nitrite (NO2-) as a terminal electron acceptor to produce nitric oxide (NO), which is then combined with ammonium (NH4+) to produce the intermediate hydrazine (N2H4) and water (H2O). Hydrazine, a very reactive molecule also used for rocket fuel, is then oxidized into nitrogen gas (N2)[6]. The half reactions may be represented as:

“NO2- + 2H+ + e- = NO + H2O (E° = +0.38V)

NO + NH4+ + 2H+ + 3e- = N2H4 + H2O (E° = +0.06V)

Mechanism of Ammonium Oxidation

N2H4 = N2 + 4H+ + 4e- (E° = -0.75V)”[5]

This metabolic pathway occurs anaerobically, something that was once considered impossible as ammonium was thought to be inert in the absence of oxygen[7]. In fact, the presence of oxygen over 2 uM inhibits the anammox pathway, which is why Scalindua respire anaerobically[5].

These reactions occur in a large membrane-bound cellular organelle called the anammoxosome, which contains an electron transport chain and an ATPase that pumps protons back into the cytoplasm from the anammoxosome lumen. It functions much like a mitochondrion in eukaryotic cells. The anammoxosome membrane is invaginated (folded in upon itself) to increase its surface area[8]. The existence of membrane-bound cellular organelles is very unusual in prokaryotes, and appears to be limited to the planctomycetes phylum[9].

Scalindua and other anammox bacteria fix carbon using carbon dioxide as a carbon source. Metagenomic analysis has revealed the presence of genes responsible for the “reductive acetyl-CoA pathway (also known as the Wood-Ljungdahl pathway) which allows for the creation of the precursor molecule acetyl CoA from carbon dioxide[10][11].  

Discovery and Distribution

Ammonium and methane are known to be relatively difficult to activate with reactions catalyzed by enzymes that make use of high-potential oxygen radicals, which are unavailable to anaerobic life leading to the assumption that both compounds where effectively inactive in low oxygen environments[12]. Throughout the 1970s and 80s, results from several independent studies exploring relationships between methane and sulfate concentrations in marine sediments found indication that anaerobic methane oxidation was in fact a widespread occurrence[12]. It was not until 1999 that the existence of aerobic ammonium oxidation was first discovered in a wastewater treatment plant in The Netherlands and given the name “anammox,” which would later prove to be a key player as part of the marine nitrogen cycle[12][13][14]. Some known anammox bacteria include Candidatus Scalindua, Kuenenia, Brocadia, Jettenia and Anammoxoglobus[15]. Of these bacteria, only Candidatus Scalindua spp. can be found in marine ecosystems[15].

During the past, many microorganisms such as anammox bacteria may have escaped discovery due to their relatively low growth rate requiring very efficient biomass retention absent from classical methods of cultivation[16]. With the use of biofilms to improve the culturability of organisms that naturally occur in biofilms in combination with the use of biomass retention to study slowly growing microorganisms under substrate limitation, a technique using sequencing batch reactors (SBR) was developed for the long-term enrichment, cultivation, and quantitative analysis of a very slowly growing microbial community[16]. Phylogenetic analysis of the first anamox bacteria discovered concluded that the organisms branched deeply into the Planctomycetes phylum, which was previously considered to be of limited environmental importance[13]. Nitrogen loses that could only be explained by the process of anammox continued to be discovered in freshwater waste treatment facilities around the world including North America, Asia, and multiple regions throughout Europe[17]. Scalindua’s role in the marine nitrogen cycle has been found to be of importance regarding the reduction of nitrate to atmospheric nitrogen in the anoxic regions of the ocean[14]. Since primary productivity in the ocean is often limited by nitrogen availability, the removal of usable nitrogen in sediments through anammox by Scalindua may significantly affect biogeochemical cycles in anoxic waters[14]. In certain regions, such as the Golfo Dulce in Costa Rica, up to %35 of atmospheric nitrogen production in the water column can be attributed to Scalindua spp[14]. In other regions such as the Black Sea, the worlds largest anoxic basin characterized by a large gradient in ammonium concentrations (high levels in deep water tapering off to only trace amounts in the suboxic zone), the apparent ammonium sink in the suboxic zone was identified to be the result of anaerobic oxidation by Scalindua spp[18].

Morphology

Organisms within the genus “Candidatus Scalindua” are classified as gram-negative chemolithoautotrophic bacteria [3]. This means that their carbon and energy largely come from inorganic sources. Furthermore, Scalindua are obligate anaerobes, so they are unable live in oxygen-rich environments [3][2].

 As with all other organisms within the order Planctomycetes, the cell wall of these organisms does not contain peptidoglycan[2][19]. Scalindua are spherical in shape, with a diameter of roughly one micrometer, and contain compartmentalized cytoplasms[2]. Furthermore, organisms within Candidatus Scalindua have two inner membranes instead of one inner, and one outer surrounding the cell wall.[20] Cells within Scalindua wagenri are oriented into compact clusters, whereas Scalindua brodae’s cells are found to be more loosely packed[2]. All Scalindua contain unique organelles called Anammoxosomes, which are membrane bound within the cytoplasm[2][21]. Anammoxosomes are where the anaerobic ammonium oxidation process occurs. The membrane that surrounds anammoxosomes in anammox bacteria contain unique lipids called “ladderane” lipids, which contain a series of cyclobutane ring structures[21]. However, all other membranes within anammox bacteria are similar to organisms within the order Planctomycetes.

Evolutionary History

According to Strous et. al., anammox-capability is the result of a singular evolutionary event. All anammox bacteria are descendents of the same ancient planctomycetes species that first evolved the anammox reaction[22]. The Scalindua genus is the most widespread of all the anammox bacteria genera described so far[23].

Currently, all anammox bacteria are thought to be members of the order Brocadiales[24].

Ecological Role

Candidatus Scalindua sp. were the only Candidatus species found in the Black Sea, the Benguela OMZ off the coast of Namibia, and the estuary in the Randers Fjord, Denmark. [25] Globally, Candidatus Scalindua has been discovered in all of the marine environments that have been studied; other marine bacteria are not this ubiquitous.[25][15]

The ideal environmental conditions, with regards to temperature, pH and salinity for “Candidatus Scalindua sp.” are: 10 to 30°C, 6.0 to 8.5 pH and 0.8% to 4.0% salinity with no activity when salinity was 0%, respectively. [26]

Marine sediments located in deep-sea methane seeps contain anammox bacteria associated with the Candidatus Scalindua sp; these bacteria likely have a substantial role in the nitrogen cycle found in the sediments.[27]

Two types of anammox bacteria, Scalindua (59% abundance) and Kuenenia (41% abundance), have been found in the non-rhizosphere area of the saltmarsh grass Spartina alterniflora while only Scalindua was present within the rhizosphere and at 1.5 times greater than the amount of anammox bacterial in the non-rhizosphere sediments.[28] Changing seasons do not affect the make-up of the anammox bacterial communities within the sediments in and around the rhizosphere; however there was always a greater abundance of the anammox bacteria within the rhizosphere, which peaks during July and October when temperature are warmest.[28] During the warmer parts of the year both communities of the anammox bacteria within and outside of the rhizosphere are more active and produce more N2 with the bacteria in the rhizosphere producing almost twice as much N2.[28]

Taxonomy

Candidatus Scalindua is closely related genetically to the other Anammox bacteria within the order Planctomycetes, such as Candidatus Brocadia and Candidatus Kuenenia.[2]. Yet, Scalindua is quite different from other genuses of Anammox bacteria on the 16s rRNA level [2]. For example, Candidatus Scalindua and Candidatus Brocadia only share 85% similar sequences [2]. Candidatus Scalindua can be further divided into three species: Scalindua brodae, Scalindua wagneri, and Scalindua sorokinii [2][29]. Scalindua is the most abundant genus of Anammox bacteria known to date, making it very important in the world’s aquatic environments. 

Applications

Scalindua wagneri are often used in wastewater treatment plants as a buffer of sorts to reduce the adverse effects of nitrification and denitrification on the local environment

[30].The use of annamox bacteria in wastewater treatment plants has a drastically reduced cost compared to previous dinitrification methods. Furthermore, it is a much more environmentally friendly method. [10]

References

Species

References

  1. ^ Schmid, Markus; Walsh, Kerry; Webb, Rick; Rijpstra, W. Irene; van de Pas-Schoonen, Katinka; Verbruggen, Mark Jan; Hill, Thomas; Moffett, Bruce; Fuerst, John; Schouten, Stefan; Sinninghe Damsté, Jaap S.; Harris, James; Shaw, Phil; Jetten, Mike; Strous, Marc (2003). "Candidatus "Scalindua brodae", sp. nov., Candidatus "Scalindua wagneri", sp. nov., Two New Species of Anaerobic Ammonium Oxidizing Bacteria". Systematic and Applied Microbiology. 26 (4): 529–538. doi:10.1078/072320203770865837. ISSN 0723-2020. PMID 14666981.
  2. ^ a b c d e f g h i j k Schmid, Markus (2003). "Candidatus "Scalindua brodae", sp. nov., Candidatus "Scalindua wagneri", sp. nov., Two New Species of Anaerobic Ammonium Oxidizing Bacteria". Systematic and Applied Microbiology. 26 [4]: 529–538.
  3. ^ a b c Awata, Takanori; Oshiki, Mamoru; Kindaichi, Tomonori; Ozaki, Noriatsu; Ohashi, Akiyoshi; Okabe, Satoshi (2017-03-08). "Physiological Characterization of an Anaerobic Ammonium-Oxidizing Bacterium Belonging to the "Candidatus Scalindua" Group". Applied and Environmental Microbiology. 79 (13): 4145–4148. doi:10.1128/AEM.00056-13. ISSN 0099-2240. PMC 3697556. PMID 23584767.{{cite journal}}: CS1 maint: PMC format (link) Cite error: The named reference ":6" was defined multiple times with different content (see the help page).
  4. ^ Kuenen, J. Gijs (2008-04-01). "Anammox bacteria: from discovery to application". Nature Reviews Microbiology. 6 (4): 320–326. doi:10.1038/nrmicro1857. ISSN 1740-1526.
  5. ^ a b c "Anammox Bacteria". Microbewiki. {{cite web}}: Cite has empty unknown parameter: |dead-url= (help)
  6. ^ K., Poole, Robert (2012-01-01). Advances in microbial physiology Volume 60. Elsevier/Academic Press. ISBN 9780123982643. OCLC 797831085.{{cite book}}: CS1 maint: multiple names: authors list (link)
  7. ^ Strous, Marc; Jetten, Mike S. M. (2004-09-13). "Anaerobic Oxidation of Methane and Ammonium". http://dx.doi.org/10.1146/annurev.micro.58.030603.123605. doi:10.1146/annurev.micro.58.030603.123605. Retrieved 2017-03-08. {{cite web}}: External link in |website= (help)
  8. ^ Niftrik, Laura van; Jetten, Mike S. M. (2012-09-01). "Anaerobic Ammonium-Oxidizing Bacteria: Unique Microorganisms with Exceptional Properties". Microbiology and Molecular Biology Reviews. 76 (3): 585–596. doi:10.1128/MMBR.05025-11. ISSN 1092-2172. PMC 3429623. PMID 22933561.{{cite journal}}: CS1 maint: PMC format (link)
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  10. ^ a b van de Vossenberg, Jack; Woebken, Dagmar; Maalcke, Wouter J; Wessels, Hans J C T; Dutilh, Bas E; Kartal, Boran; Janssen-Megens, Eva M; Roeselers, Guus; Yan, Jia (2017-03-08). "The metagenome of the marine anammox bacterium 'Candidatus Scalindua profunda' illustrates the versatility of this globally important nitrogen cycle bacterium". Environmental Microbiology. 15 (5): 1275–1289. doi:10.1111/j.1462-2920.2012.02774.x. ISSN 1462-2912. PMC 3655542. PMID 22568606.{{cite journal}}: CS1 maint: PMC format (link)
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  13. ^ a b Jetten, Mike S. M.; Strous, Marc; Fuerst, John A.; Kramer, Evelien H. M.; Logemann, Susanne; Muyzer, Gerard; Pas-Schoonen, Katinka T. van de; Webb, Richard; Kuenen, J. Gijs. "http://www.nature.com/doifinder/10.1038/22749". Nature. 400 (6743): 446–449. doi:10.1038/22749. {{cite journal}}: External link in |title= (help)
  14. ^ a b c d Dalsgaard, Tage; Canfield, Donald E.; Petersen, Jan; Thamdrup, Bo; Acuña-González, Jenaro. "N2 production by the anammox reaction in the anoxic water column of Golfo Dulce, Costa Rica". Nature. 422 (6932): 606–608. doi:10.1038/nature01526.
  15. ^ a b c Woebken, Dagmar; Lam, Phyllis; Kuypers, Marcel M. M.; Naqvi, S. Wajih A.; Kartal, Boran; Strous, Marc; Jetten, Mike S. M.; Fuchs, Bernhard M.; Amann, Rudolf (2008-11-01). "A microdiversity study of anammox bacteria reveals a novel Candidatus Scalindua phylotype in marine oxygen minimum zones". Environmental Microbiology. 10 (11): 3106–3119. doi:10.1111/j.1462-2920.2008.01640.x. ISSN 1462-2920.
  16. ^ a b Strous, M.; Heijnen, J. J.; Kuenen, J. G.; Jetten, M. S. M. (1998-11-01). "The sequencing batch reactor as a powerful tool for the study of slowly growing anaerobic ammonium-oxidizing microorganisms". Applied Microbiology and Biotechnology. 50 (5): 589–596. doi:10.1007/s002530051340. ISSN 0175-7598.
  17. ^ Schmid, Markus C.; Maas, Bart; Dapena, Ana; Pas-Schoonen, Katinka van de; Vossenberg, Jack van de; Kartal, Boran; Niftrik, Laura van; Schmidt, Ingo; Cirpus, Irina (2005-04-01). "Biomarkers for In Situ Detection of Anaerobic Ammonium-Oxidizing (Anammox) Bacteria". Applied and Environmental Microbiology. 71 (4): 1677–1684. doi:10.1128/AEM.71.4.1677-1684.2005. ISSN 0099-2240. PMC 1082507. PMID 15811989.{{cite journal}}: CS1 maint: PMC format (link)
  18. ^ Kuypers, Marcel M. M.; Sliekers, A. Olav; Lavik, Gaute; Schmid, Markus; Jørgensen, Bo Barker; Kuenen, J. Gijs; Damsté, Jaap S. Sinninghe; Strous, Marc; Jetten, Mike S. M. "Anaerobic ammonium oxidation by anammox bacteria in the Black Sea". Nature. 422 (6932): 608–611. doi:10.1038/nature01472.
  19. ^ Lindsay, M.R, (2001). "Cell compartmentalisation in planctomycetes: novel types of structural organisation for the bacterial cell". Archives of Microbiology. 175 [6]: 413–429.{{cite journal}}: CS1 maint: extra punctuation (link) CS1 maint: multiple names: authors list (link)
  20. ^ van Niftrick, Laura A. (2004). "The anammoxosome: an intracytoplasmic compartment in anammox bacteria". FEMS Microbiology Letters. 233 (1): 7–13.
  21. ^ a b Sinninghe, Damste (2002). "Linearly concatenated cyclobutane lipids form a dense bacterial membrane". Nature. 419: 708–712.
  22. ^ Strous, Marc; Jetten, Mike S. M. (2004-09-13). "Anaerobic Oxidation of Methane and Ammonium". http://dx.doi.org/10.1146/annurev.micro.58.030603.123605. doi:10.1146/annurev.micro.58.030603.123605. Retrieved 2017-03-08. {{cite web}}: External link in |website= (help)
  23. ^ Schmid, Markus; Walsh, Kerry; Webb, Rick; Rijpstra, W. Irene C.; van de Pas-Schoonen, Katinka; Verbruggen, Mark Jan; Hill, Thomas; Moffett, Bruce; Fuerst, John (2003-11-01). "Candidatus "Scalindua brodae", sp. nov., Candidatus "Scalindua wagneri", sp. nov., two new species of anaerobic ammonium oxidizing bacteria". Systematic and Applied Microbiology. 26 (4): 529–538. ISSN 0723-2020. PMID 14666981.
  24. ^ Speth, Daan R.; Russ, Lina; Kartal, Boran; op den Camp, Huub J. M.; Dutilh, Bas E.; Jetten, Mike S. M. (2015-01-08). "Draft Genome Sequence of Anammox Bacterium "Candidatus Scalindua brodae," Obtained Using Differential Coverage Binning of Sequencing Data from Two Reactor Enrichments". Genome Announcements. 3 (1). doi:10.1128/genomeA.01415-14. ISSN 2169-8287. PMC 4290996. PMID 25573945.{{cite journal}}: CS1 maint: PMC format (link)
  25. ^ a b Schmid, Markus C.; Risgaard-Petersen, Nils; Van De Vossenberg, Jack; Kuypers, Marcel M. M.; Lavik, Gaute; Petersen, Jan; Hulth, Stefan; Thamdrup, Bo; Canfield, Don (2007-06-01). "Anaerobic ammonium-oxidizing bacteria in marine environments: widespread occurrence but low diversity". Environmental Microbiology. 9 (6): 1476–1484. doi:10.1111/j.1462-2920.2007.01266.x. ISSN 1462-2920.
  26. ^ Awata, Takanori; Oshiki, Mamoru; Kindaichi, Tomonori; Ozaki, Noriatsu; Ohashi, Akiyoshi; Okabe, Satoshi (2013-07-01). "Physiological Characterization of an Anaerobic Ammonium-Oxidizing Bacterium Belonging to the "Candidatus Scalindua" Group". Applied and Environmental Microbiology. 79 (13): 4145–4148. doi:10.1128/AEM.00056-13. ISSN 0099-2240. PMC 3697556. PMID 23584767.{{cite journal}}: CS1 maint: PMC format (link)
  27. ^ Shao, Sudong; Luan, Xiwu; Dang, Hongyue; Zhou, Haixia; Zhao, Yakun; Liu, Haitao; Zhang, Yunbo; Dai, Lingqing; Ye, Ying (2014-02-01). "Deep-sea methane seep sediments in the Okhotsk Sea sustain diverse and abundant anammox bacteria". FEMS Microbiology Ecology. 87 (2): 503–516. doi:10.1111/1574-6941.12241. ISSN 0168-6496.
  28. ^ a b c Zheng, Yanling; Hou, Lijun; Liu, Min; Yin, Guoyu; Gao, Juan; Jiang, Xiaofen; Lin, Xianbiao; Li, Xiaofei; Yu, Chendi (2016-09-01). "Community composition and activity of anaerobic ammonium oxidation bacteria in the rhizosphere of salt-marsh grass Spartina alterniflora". Applied Microbiology and Biotechnology. 100 (18): 8203–8212. doi:10.1007/s00253-016-7625-2. ISSN 0175-7598.
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