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Stable-isotope probing

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abundance of elements in the DNA. For example, the difference in mass between O and O (two atomic mass units) is twice that between C and C (one atomic mass unit), so incorporation of O into DNA will cause a larger per atom density shift than will incorporation of C. Conversely, DNA contains nearly twice as many carbon atoms (11.25 per base, on average) as oxygen atoms (6 per base), so at equivalent labeling (e.g., 50 atom percent C or O), DNA labeled with O will be only slightly more dense than DNA fully labeled with C. Similarly, nitrogen is less abundant in DNA (3.75 atoms per base, on average), so a weaker DNA buoyant density shift is observed with N- versus C-labeled or O-labeled substrates. Larger buoyant density shifts are observed when multiple isotope tracers are used. Because density shifts as a predictable function of the change in mass caused by isotope assimilation, stable isotope probing can be modeled to estimate the amount of isotope incorporation, an approach called quantitative stable isotope probing (qSIP), which has been applied to microbial communities in soils, marine sediments, and decomposing leaves to compare rates of growth and substrate assimilation among different microbial taxa.
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When DNA is the biomarker, SIP can be performed using isotopically labeled C, H, O, or N, though C is used most often. The density shift is proportional to the change in density in the DNA, which depends on the difference in mass between the rare and common isotopes for a given element, and on the
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and which were using carbohydrates more recently produced from photosynthesis. SIP with O-labeled water can be used to find out which organisms are actively growing, because oxygen from water is incorporated into DNA (and RNA) during synthesis.
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with the heavier isotopes incorporated into them can be separated from biomarkers containing the more naturally abundant lighter isotope by
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with C is then separated from DNA with C by centrifugation.
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the DNA identifies which organisms were consuming existing
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by microorganisms. A substrate is enriched with a heavier
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Jiang B, Jin N, Xing Y, Su Y, Zhang D (November 2018).
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Stable isotope labeling by amino acids in cell culture
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can be used to find out which organisms are actively
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Microbiology 7: 664:10.1016/j.ymeth.2018.05.022 80: 10: 823: 802:Environmental microbiology 760:21.11116/0000-0001-C275-0 625:10.1016/j.tim.2018.06.004 507:10.1038/s41396-019-0373-4 170:10.1007/s00248-006-9125-x 441:10.1128/msphere.00085-21 323:Microbiological Research 45:isopycnic centrifugation 787:Microbiology techniques 573:10.1111/1758-2229.12475 613:Trends in Microbiology 33:biogeochemical cycling 27:for tracing uptake of 17:Stable-isotope probing 383:10.1128/AEM.02280-15 281:10.1128/AEM.02021-06 23:) is a technique in 564:2016EnvMR...8..975H 499:2019ISMEJ..13.1546C 375:2015ApEnM..81.7570H 272:2007ApEnM..73.2541S 213:2000Natur.403..646R 162:2007MicEc..53..435N 119:10.1038/nrmicro1162 369:(21): 7570–7581. 150:Microbial Ecology 58:photosynthesizing 25:microbial ecology 814: 772: 762: 752: 727: 702:(7): 1025–1048. 693: 683: 646: 636: 619:(12): 999–1007. 594: 593: 575: 543: 537: 536: 526: 493:(6): 1546–1559. 487:The ISME Journal 478: 472: 471: 453: 443: 419: 413: 412: 402: 353: 347: 346: 318: 312: 311: 293: 283: 266:(8): 2541–2546. 247: 241: 240: 221:10.1038/35001054 196: 190: 189: 145: 139: 138: 102: 822: 821: 817: 816: 815: 813: 812: 811: 777: 776: 775: 691: 602: 600:Further reading 597: 544: 540: 479: 475: 434:(5): e0008521. 420: 416: 354: 350: 319: 315: 255: 248: 244: 207:(6770): 646–9. 197: 193: 146: 142: 103: 99: 95: 83: 54: 47:. 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Index

microbial ecology
nutrients
biogeochemical cycling
stable isotope
Biomarkers
isopycnic centrifugation

CO2
photosynthesizing
DNA
Sequencing
carbohydrates
Stable isotope labeling by amino acids in cell culture
doi
10.1038/nrmicro1162
PMID
15886694
S2CID
24051877
Bibcode
2007MicEc..53..435N
doi
10.1007/s00248-006-9125-x
PMID
17072677
S2CID
9417066
Bibcode
2000Natur.403..646R
doi

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