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Isotope analysis

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Isotope analysis

Magnetic sector mass spectrometer used in isotope ratio analysis, through thermal ionization.

Isotope analysis is the identification of isotopic signature, the distribution of certain stable isotopes and chemical elements within chemical compounds. This can be applied to a food web to make it possible to draw direct inferences regarding diet, trophic level, and subsistence. Variations in isotope ratios from isotopic fractionation are measured using mass spectrometry, which separates the different isotopes of an element on the basis of their mass-to-charge ratio.

The ratios of isotopic oxygen are also differentially affected by global weather patterns and regional topography as moisture is transported. Areas of lower humidity cause the preferential loss of 18O water in the form of vapor and precipitation. Furthermore, evaporated 16O water returns preferentially to the atmospheric system as it evaporates and 18O remains in liquid form or is incorporated into the body water of plants and animals.

Contents

  • Tissue affected 1
  • Applications 2
    • Archaeology 2.1
      • Reconstructing palaeodiet 2.1.1
      • Sourcing archaeological materials 2.1.2
    • Ecology 2.2
      • Stable isotope analysis in aquatic ecosystems 2.2.1
        • 13C 2.2.1.1
        • 34S 2.2.1.2
        • 15N 2.2.1.3
    • Forensics 2.3
    • Geology 2.4
    • Hydrology 2.5
    • Paleoclimatology 2.6
  • References 3
  • External links 4

Tissue affected

Isotopic oxygen is incorporated into the body primarily through ingestion at which point it is used in the formation of, for archaeological purposes, bones and teeth. The oxygen is incorporated into the hydroxylcarbonic apatite of bone and tooth enamel.

Bone is continually remodelled throughout the lifetime of an individual. Although the rate of turnover of isotopic oxygen in hydroxyapatite is not fully known, it is assumed to be similar to that of collagen; approximately 10 years. Consequently, should an individual remain in a region for 10 years or longer, the isotopic oxygen ratios in the bone hydroxyapatite would reflect the oxygen ratios present in that region.

Teeth are not subject to continual remodelling and so their isotopic oxygen ratios remain constant from the time of formation. The isotopic oxygen ratios, then, of teeth represent the ratios of the region in which the individual was born and raised. Where deciduous teeth are present, it is also possible to determine the age at which a child was weaned. Breast milk production draws upon the body water of the mother, which has higher levels of 18O due to the preferential loss of 16O through sweat, urine, and expired water vapour.

While teeth are more resistant to chemical and physical changes over time, both are subject to post-depositional diagenesis. As such, isotopic analysis makes use of the more resistant phosphate groups, rather than the less abundant hydroxyl group or the more likely diagenetic carbonate groups present.

Applications

Isotope analysis has widespread applicability in the natural sciences. These include numerous applications in the biological, earth and environmental sciences.

Archaeology

Reconstructing palaeodiet

Tissue remains recovered from archaeological sites can be analysed isotopically. Carbon and nitrogen isotope composition are used to reconstruct diet, and oxygen isotopes are used to determine geographic origin and paleoenvironment. Strontium and lead isotopes can be used to understand population movements, like migration and seasonal mobility.[1] It is common to combine elements in isotopic analysis in archaeology to reconstruct diet, change in water source, migration, and cultural interaction. For example, archaeologists were able to confirm that population growth within the upper Min River Valley in Thailand during the Iron Age was due to local factors rather than immigration from other areas.[2]

Carbon isotopes enter the food chain as herbivores consume plants, and oxygen isotopes enter the food chain from consuming meteoric water and water from the diet. Examining the diagenesis that may affect the original isotopic signal. It is also important for the researcher to know the variations of isotopes within individuals, between individuals, and over time.

Sourcing archaeological materials

Isotope analysis has been particularly useful in archaeology as a means of characterization. Characterization of artifacts involves determining the isotopic composition of possible source materials such as metal ore bodies and comparing these data to the isotopic composition of analyzed artifacts. A wide range of archaeological materials such as metals, glass and lead-based pigments have been sourced using isotopic characterization.[4] Particularly in the Bronze Age Mediterranean Lead Isotope Analysis has been a useful tool for determining the sources of metals and an important indicator of trade patterns. Interpretation of Lead Isotope Data is, however, often contentious and faces numerous instrumental and methodological challenges.[5] Problems such as the mixing and re-using of metals from different sources, limited reliable data and contamination of samples can be difficult problems in interpretation.

Ecology

All biologically active elements exist in a number of different isotopic forms, of which two or more are stable. For example most carbon is present as 12C, with approximately 1% being 13C. The ratio of the two isotopes may be altered by biological and geophysical processes, and these differences can be utilized in a number of ways by ecologists. The main elements used in isotope ecology are carbon, nitrogen, oxygen, hydrogen and sulfur.

Analysis of the ratio of 18O to 16O in the shells of the Colorado Delta clam was used to assess the historical extent of the estuary in the Colorado River Delta prior to construction of upstream dams.[6]

Stable isotope analysis in aquatic ecosystems

Stable isotopes have become a popular method for understanding aquatic ecosystems because they can help scientists in understanding source links and process information in marine food webs. These analysis can also be used to a certain degree in terrestrial systems. Certain isotopes can signify distinct primary producers forming the bases of food webs and trophic level positioning. The stable isotope compositions are expressed in terms of delta values (δ) in permil (‰), i.e. parts per thousand differences from a standard. They express the proportion of an isotope that is in a sample. The values are expressed as:

δX = [(Rsample / Rstandard) – 1] x 103

where X represents the isotope of interest (e.g., 13C) and R represents the ratio of the isotope of interest and its natural form (e.g., 13C/12C).[7] Higher (less negative) delta values indicate increases in a sample's isotope of interest, relative to the standard, and lower (or more negative) values indicate decreases. The standard reference materials for carbon, nitrogen, and sulfur are Pee Dee Belamnite limestone, nitrogen gas in the atmosphere, and Cañon Diablo meteorite respectively. Analysis is usually done using a mass spectrometer, detecting small differences between gaseous elements. Analysis of a sample can cost anywhere from $30 to $100.[7] Stable isotopes assist scientists in analyzing animal diets and food webs by examining the animal tissues that bear a fixed isotopic enrichment or depletion vs. the diet. Muscle or protein fractions have become the most common animal tissue used to examine the isotopes because they represent the assimilated nutrients in their diet. The main advantage to using stable isotope analysis as opposed to stomach content observations is that no matter what the status is of the animal's stomach (empty or not), the isotope tracers in the tissues will give us an understanding of its trophic position and food source.[8] The three major isotopes used in aquatic ecosystem food web analysis are 13C, 15N and 34S. While all three indicate information on trophic dynamics, it is common to perform analysis on at least two of the previously mentioned 3 isotopes for better understanding of marine trophic interactions and for stronger results.

13C

  • IsoSource. Stable isotope mixing model for an excess number of sources (Visual Basic), (Phillips and Gregg, 2003).
  • MixSIR: A Bayesian Stable Isotope Mixing Model. MixSIR is a free graphical user interface (GUI) program built on the MATLAB platform that carries out Bayesian analysis of stable isotope mixing models using sampling-importance-resampling (SIR). (Moore and Semmens, 2008).
  • SIAR - Stable isotope analysis in R.. Bayesian mixing model package for the R environment. Parnell, A., Inger, R., Bearhop, S., Jackson, A.
  • SISUS: Stable Isotope Sourcing using Sampling. Stable Isotope Sourcing using Sampling (SISUS) (Erhardt, Wolf, and Bedrick, In Prep.) provides a more efficient algorithm to provide solutions to the same problem as the Phillips and Gregg (2003) IsoSource model and software for source partitioning using stable isotopes.
  • IsotopeR. Bayesian stable isotope mixing model that incorporates measurement error, concentration dependence and other features in a single package. IsotopeR runs in the R environment. (Hopkins and Ferguson, 2011)

External links

  1. ^ Carlson, A. K. 1996. Lead Isotope Analysis of Human Bone for Addressing Cultural Affinity: a Case Study from Rocky Mountain House, Alberta. Journal of Archaeological Science 23: 557–567.
  2. ^ Cox, K. J., Bentley, R. A., Tayles, N., Buckley, H. R., Macpherson, C. G., & Cooper, M. J. (2011). Intrinsic or extrinsic population growth in Iron Age northeast Thailand? The evidence from isotopic analysis. Journal of Archaeological Science, 38(3)
  3. ^ Cox, K. J., Bentley, R. A., Tayles, N., Buckley, H. R., Macpherson, C. G., & Cooper, M. J. (2011). Intrinsic or extrinsic population growth in Iron Age northeast Thailand? The evidence from isotopic analysis. Journal of Archaeological Science, 38(3), pp. 665-671
  4. ^ Shortland, A. J. 2006. Application of Lead Isotope Analysis to a Wide Range of Late Bronze Age Egyptian Materials. Archaeometry. 48(4): 657-669.
  5. ^ Budd, P., Haggerty, R., Pollard, A. M., Scaife, B. and Thomas, R. G. 1996. Rethinking the quest for provenance. (lead isotope analysis). Antiquity 70(267): 168-175.
  6. ^ K.W, C (2001), "Macrofaunal and isotopic estimates of the former extent of the Colorado River Estuary, upper Gulf of California, Mexico" (PDF), Journal of Arid Environments 49 (1): 183–193,  
  7. ^ a b Fry, B., Peterson, B.J. 1987. Stable Isotopes in Ecosystem Studies. Annual Review of Ecology, Evolution and Systematics 18:293-320.
  8. ^ a b c d e f Michener, L. K. a. R. 2007. Stable isotope ratios as tracers in marine food webs: and update. Pages 238-282 Stable Isotopes and Ecology in Environmental Science. Blackwell Publishing, Oxford, UK.
  9. ^ *Fry, B. 1983. Fish and shrimp migrations in the northern Gulf of Mexico analyzed using stable C, N and S isotope ratios. Fisheries Bulletin 81:7890801.
  10. ^ Daniel, K. W. S. a. R. M. 1978. Fractionation of nitrogen isotopes by animals: a further complication to the use of variations in the natural abundance of 15N for tracer studies. Journal of Agricultural Science 90:7-9.
  11. ^ a b Sture Hansson, J. E. H., Ragnar Elmgren, Ulfa Larsson, Brian Fry, Sif Johansson. 1997. The stable nitrogen isotope ratio as a marker of food-web interactions and fish migration. Ecology 78:2249-2257.
  12. ^ a b C.W. Kreitler, S. R. a. B. G. K. 1978. N15/N14 ratios of ground-water nitrate, Long Island, New York. Ground Water 16:404-409.
  13. ^ Valiela, J. W. M. a. I. 1998. Linking Nitrogen in Estuarine Producers to Land-derived sources. Limnology and Oceanography 43:577-585.
  14. ^ R.H. Carmichael, T. H., I. Valiela, R.H. Michener. 2008. Nitrogen stable isotopes in the shell of Mercenaria mercenaria trace wastewater inputs from watersheds to estuarine ecosystems. Aquatic Biology 4:99-111.
  15. ^ J.W. McClelland, I. V. a. R. H. M. 1997. Nitrogen-stable isotope signatures in estuarine food webs: A record of increasing urbanization in coastal watersheds. Limnology and Oceanography 42:930-937.
  16. ^ S. Black., Crime Scene Analysis, Reading University, 2008
  17. ^ P. White., Crime Scene to Court: The Essentials of Forensic Science; Second Edition, Royal Society of Chemistry, 2004
  18. ^ J.R. Ehleringer, J. Casale, D.A. Cooper, M.J. Lott., Sourcing Drugs With Stable Isotopes - [2]

References

Oxygen isotopes preserve a record of the effects of the Milankovitch cycles on climate change during the Quaternary, revealing an approximately 100,000-year cyclicity in the Earth's climate.

The ratio of 18O to 16O in ice and deep sea cores is temperature dependent, and can be used as a proxy measure for reconstructing climate change. During colder periods of the Earth's history (glacials) such as during the Quaternary. Similarly, ice cores on land are enriched in the heavier 18O relative to 16O during warmer climatic phases (interglacials) as more energy is available for the evaporation of the heavier 18O isotope. The oxygen isotope record preserved in the ice cores is therefore a `mirror` of the record contained in ocean sediments.

Paleoclimatology

Hydrology

Geology

Stable isotopic analysis has also been used in the identification of drug trafficking routes. Isotopic abundances are different in morphine grown from poppies in South-east Asia versus poppies grown in South-West Asia. The same is applied to cocaine that is derived from Bolivia and that from Colombia.[18]

Isotope analysis can be used by forensic investigators to determine whether two or more samples of explosives are of a common origin. Most high explosives contain carbon, hydrogen, nitrogen and oxygen atoms and thus comparing their relative abundances of isotopes can reveal the existence of a common origin. Researchers have also shown that analysis of the 12C/13C ratios can locate the country of origin for a given explosive.

A recent development in forensic science is the isotopic analysis of hair strands. Hair has a recognisable growth rate of 9-11mm[16] per month or 15 cm per year.[17] Hair growth is primarily a function of diet, especially drinking water intake. The stable isotopic ratios of drinking water are a function of location, and the geology that the water percolates through. 87Sr, 88Sr and oxygen isotope variations are different all over the world. These differences in isotopic ratio are then biologically 'set' in our hair as it grows and it has therefore become possible to identify recent geographic histories by the analysis of hair strands. For example, it could be possible to identify whether a terrorist suspect had recently been to a particular location from hair analysis. This hair analysis is a non-invasive method which is becoming very popular in cases that DNA or other traditional means are bringing no answers.

Forensics

[15]N because it is a lighter element and easier to metabolize. Thus, due to bacteria's preference when performing 15N as opposed to 14 For bacteria, it is more convenient for them to uptake [12]N than the nitrate that is found in natural soils in near shore zones.15N values have become commonly used in distinguishing between land derived and natural sources of nutrients. As water travels from septic tanks to aquifers, the nitrogen rich water is delivered into coastal areas. Waste-water nitrate has higher concentrations of 15 In addition to trophic positioning of organisms, δ

Nitrogen isotopes indicate the trophic level position of various marine organisms (reflective of the time the tissue samples were taken). There is a larger enrichment component with δ15N because its retention is higher than that of 14N. This can be seen by analyzing the waste of organisms.[8] Cattle urine has shown that there is a depletion of 15N relative to the diet.[10] As organisms eat each other, the 15N isotopes are transferred to the predators. Thus, organisms higher in the zooplankton, mysids, sprat, smelt and herring,) there was an apparent fractionation of 2.4‰ between consumers and their apparent prey.[11]

15N

While there is no enrichment of 34S between trophic levels, the stable isotope can be useful in distinguishing benthic vs. pelagic producers and marsh vs. phytoplankton producers.[8] Similar to 13C, it can also help distinguish between different phytoplankton as the key primary producers in food webs. The differences between seawater sulfates and sulfides (~21‰ vs -10‰) aid scientists in the discriminations. Sulfur tends to be more plentiful in less aerobic areas, such as benthic systems and marsh plants, than the pelagic and more aerobic systems. Thus, in the benthic systems, there are smaller δ34S values.[8]

34S

[9]

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