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An insect isoscape of UK and Ireland

Profile image of Jason NewtonJason Newton

2021, Rapid communications in mass spectrometry : RCM

https://doi.org/10.1002/RCM.9126
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Abstract

RATIONALE The study of insect migration is problematic due to the small size of insects. Stable isotope analysis can be used to elucidate movement, either by geographic assignment of location of a species, or by simply distinguishing migrant from resident populations. There are few isoscapes of any kind in the UK/Ireland available for interrogation. Thus, I have measured stable isotope ratios (of H, C, N and S) of 299 individuals of the non-migratory Brimstone moth (Opisthograptis luteolata) collected from 93 locations around the UK and Ireland by citizen scientists. METHODS After removing lipids, stable isotope ratios were measured by continuous flow isotope ratio mass spectrometry, using either a conventional elemental analyser (C, N and S) or a high temperature, thermal conversion elemental analyser in reductive mode. RESULTS Maps (isoscapes) were constructed that illustrate the stable isotope spatial distribution of this insect. These are the first isoscapes of H, C, N and S of ...

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References (59)

  1. Chapman JW, Lim KS, Reynold DR. The significance of midsummer movements of Autographa gamma: Implications for a mechanistic understanding of orientation behavior in a migrant moth. Curr Zool. 2013;59(3):360-370. https://doi.org/10.1093/czoolo/59.3.360
  2. Holland R, Wikelski M, Wilcove DS. How and why do insects migrate? Science. 2006;313(5788):794-796. https://doi.org/10.1126/ science.1127272
  3. Monarch Watch Tagging Program, https://www.monarchwatch.org
  4. Brindza LJ, Brower LP, Davis AK, Van Hook T. Comparative success of monarch butterfly migration to overwintering sites in Mexico from inland and coastal sites in Virginia. J Lepid Soc. 2008;62:189-200.
  5. Wikelski M, Moskowitz D, Adelman JS, Cochran J, Wilcove DS, May ML. Simple rules guide dragonfly migration. Biol Lett. 2006;22(3): 325-329. https://doi.org/10.1098/rsbl.2006.0487
  6. Kissling WD, Pattemore DE, Hagen M. Challenges and prospects in the telemetry of insects. Biol Rev. 2014;89(3):511-530. https://doi. org/10.1111/brv.12065
  7. Newton J. Stable isotopes as tools in ecological research. In: Encyclopedia of Life Sciences; 2016:1-8 10.1002/9780470015902. a0021231.pub2.
  8. Hobson KA, Wassenaar LI. Tracking animal migration with stable isotopes. 2nded. Academic Press; 2019 ISBN: 978-0-12-814723-8.
  9. Wassenaar LI, Hobson KA. Natal origins of migratory monarch butterflies at wintering colonies in Mexico: New isotopic evidence. Proc Natl Acad Sci. 1998;95(26):15436-15439. https://doi.org/10. 1073/pnas.95.26.15436
  10. Hobson K, Wassenaar L, Taylor O. Stable isotopes (δD and δ 13 C) are geographic indicators of natal origins of monarch butterflies in eastern North America. Oecologia. 1999;120(3):397-404. https://doi. org/10.1007/s004420050872
  11. Flockhart DTT, Wassenaar LI, Martin TG, Hobson KA, Wunder MB, Norris DR. Tracking multi-generational colonization of the breeding grounds by monarch butterflies in eastern North America. Proc R Soc B: Biol Sci. 2013;280(1768):20131087. https://doi.org/10.1098/rspb. 2013.1087
  12. Hobson KA, Kardynal KJ, Koehler G. Expanding the isotopic toolbox to track monarch butterfly (Danaus plexippus) origins and migration: On the utility of stable oxygen isotope (δ 18 O) measurements. Front Ecol Evol. 2019;7(224):1-7. https://doi.org/10.3389/fevo.2019. 00224
  13. Stefanescu C, Soto DX, Talavera G, Vila R, Hobson KA. Long-distance autumn migration across the Sahara by painted lady butterflies: Exploiting resource pulses in the tropical savannah. Biol Lett. 2016; 12(10):20160561. https://doi.org/10.1098/rsbl.2016.0561
  14. Talavera G, Bataille CP, Benyamini D, Gascoigne-Pees M, Vila R. Round-trip across the Sahara: Afrotropical painted lady butterflies recolonize the Mediterranean in early spring. Biol Lett. 2018;14(6): 20180274. https://doi.org/10.1098/rsbl.2018.0274
  15. Hallworth MT, Marra PP, McFarland KP, Zahendra S, Studds CE. Tracking dragons: Stable isotopes reveal the annual cycle of a long- distance migratory insect. Biol Lett. 2018;14(12):20180741. https:// doi.org/10.1098/rsbl.2018.0741
  16. Hobson KA, Anderson RC, Soto DX, Wassenaar LI. Isotopic evidence that dragonflies (Pantala flavescens) migrating through the Maldives come from the northern Indian subcontinent. PLoS ONE. 2012;7(12): e52594. https://doi.org/10.1371/journal.pone.0052594
  17. Hobson KA, Jinguji H, Ichikawa Y, Kusack JW, Anderson RC. Long- distance migration of the globe skimmer dragonfly to Japan revealed using stable hydrogen (δ 2 H) isotopes. Environ Entomol. 2020;50(1): 247-255. https://doi.org/10.1093/ee/nvaa147
  18. Jewell C. Insect migration in a changing climate. PhD thesis, University of York. 2009.
  19. Hobson KA, Kusack JW, Mora-Alvarez BX. Origins of six species of butterflies migrating through northeastern Mexico: New insights from stable isotope (δ 2 H) analyses and a call for documenting butterfly migrations. Diversity. 2021;13(3):102. https://doi.org/10. 3390/d13030102
  20. West JB, Bowen GJ, Dawson TE, Tu KP (Eds). Isoscapes - Understanding Movement, Pattern, and Process on Earth through Isotope Mapping. Springer; 2010 ISBN 978-90-481-3354-3.
  21. IAEA/WMO. Global Network of Isotopes in Precipitation. The GNIP Database. 2011. Available at: http://www.iaea.org/water22
  22. Bowen GJ, Liu Z, Vander Zanden HB, Zhao L, Takahashi G. Geographic assignment with stable isotopes in IsoMAP. Methods Ecol Evol. 2014;5:201-206. https://doi.org/10.1111/2041-210X.1214723
  23. Hoogewerff J, Kemp HF, Leng MJ, Meier-Augenstein W. Spatial variability of 2 H and 18 O composition of meteoric freshwater lakes in Scotland. Isot Environ Health Stud. 2019;55(3):237-253. https://doi. org/10.1080/10256016.2019.1609958
  24. Stack P, Rock L. A δ 34 S isoscape of total sulphur in soils across Northern Ireland. Appl Geochem. 2011;26(8):1478-1487. https://doi. org/10.1016/j.apgeochem.2011.05.021
  25. Hobson KA, Plint T, Serrano EG, Alvarez XM, Ramirez I, Longstaffe FJ. Within-wing isotopic (δ 2 H, δ 13 C, δ 15 N) variation of monarch butterflies: Implications for studies of migratory origins and diet. Animal Migr. 2017;4(1):8-14. https://doi.org/10.1515/ami- 2017-0002
  26. Michalik A, McGill RAR, Furness RW, Eggers T, van Noordwijk HJ, Quillfeldt P. Black and white -does melanin change the bulk carbon and nitrogen isotope values of feathers? Rapid Commun Mass Spectrom. 2010;24(7):875-878. https://doi.org/10.1002/rcm.4462
  27. Wassenaar LI, Hobson KA, Sisti L. An online temperature-controlled vacuum-equilibration preparation system for the measurement of δ 2 H values of non-exchangeable-H and of δ 18 O values in organic materials by isotope-ratio mass spectrometry. Rapid Commun Mass Spectrom. 2015;29(5):397-407. https://doi.org/10.1002/rcm.7118
  28. Soto DX, Koehler G, Wassenaar LI, Hobson KA. Re-evaluation of the hydrogen stable isotopic composition of keratin calibration standards for wildlife and forensic science applications. Rapid Commun Mass Spectrom. 2017;31(14):1193-1203. https://doi.org/10.1002/ rcm.7893
  29. Gehre M, Hoefling R, Kowski P, Strauch G. Sample preparation device for quantitative hydrogen isotope analysis using chromium metal. Anal Chem. 1996;68(24):4414-4417. https://doi.org/10.1021/ ac9606766
  30. Wassenaar LI, Hobson KA. Comparative equilibration and online technique for determination of non-exchangeable hydrogen of keratins for use in animal migration studies. Isot Environ Health Stud. 2003; 39(3):211-217. https://doi.org/10.1080/1025601031000096781
  31. Met Office, Hollis D, McCarthy M, Kendon M, Legg T, Simpson I. HadUK-Grid Gridded Climate Observations on a 1km grid over the UK, v1.0.0.0 (1862-2017). Centre for Environmental Data Analysis, 14 November 2019. https://doi.org/10.5285/ 2a62652a4fe6412693123dd6328f6dc8
  32. Bowen GJ. The online isotopes in precipitation calculator, version 3.1. 2017. http://www.waterisotopes.org
  33. Bowen GJ, Revenaugh J. Interpolating the isotopic composition of modern meteoric precipitation. Water Resour Res. 2003;39(10):1299. https://doi.org/10.1029/2003WR002086
  34. Wood S. Generalized Additive Models: An Introduction with R. CRC Press; 2017.
  35. R Core Team. R: A Language and Environment for Statistical Computing. R Foundation for Statistical Computing, Vienna, Austria, 2016. ISBN: 3-900051-07-0 https://www.R-project.org/
  36. Hobson KA, Wassenaar LI. Linking brooding and wintering grounds of neotropical migrant songbirds using stable hydrogen isotopic analysis of feathers. Oecologia. 1997;109(1):142-148. https://doi.org/10. 1007/s004420050068
  37. Hobson KA, Doward K, Kardynal KJ, McNeil JN. Inferring origins of migrating insects using isoscapes: A case study using the true armyworm, Mythimna unipuncta, in North America. Ecol Entomol. 2018;43(3):332-341. https://doi.org/10.1111/een.12505
  38. Henwood B, Sterling P. Field guide to the caterpillars of Great Britain and Ireland. Bloomsbury Publishing; 2020 ISBN: 9781472933560.
  39. Amundson R, Austin AT, Schuur EA, et al. Global patterns of the isotopic composition of soil and plant nitrogen. Global Biogeochem Cycles. 2003;17(1). https://doi.org/10.1029/2002GB001903
  40. Craine JM, Elmore AJ, Aidar MPM, et al. Global patterns of foliar nitrogen isotopes and their relationships with climate, mycorrhizal fungi, foliar nutrient concentrations, and nitrogen availability. New Phytol. 1991;183(4):980-992. https://doi.org/10.1111/j.1469-8137. 2009.02917.x
  41. Vallano DM, Sparks JP. Foliar δ 15 N values as indicators of foliar uptake of atmospheric nitrogen pollution. Terrestrial Ecol. 2007;1: 93-109. https://doi.org/10.1016/S1936-7961(07)01007-X
  42. Galloway JN, Dentener FJ, Capone DG, et al. Nitrogen cycles: Past, present, and future. Biogeochem. 2004;70(2):153-226.
  43. Vogel JC. Recycling of CO 2 in a forest environment. Oecologia Plantarum. 1978;13:89-94.
  44. Skou P, Sihvonen P, Ennominae I. In: Hausmann A, ed. The Geometrid Moths of Europe. Vol.5. Leiden: Brill; 2015: 1-657.
  45. Botanical Society of Britain and Ireland BSBI's Distribution Database. Available: https://database.bsbi.org/
  46. Miller JM, Williams RJ, Farquhar GD. Carbon isotope discrimination by a sequence of eucalyptus species along a subcontinental rainfall gradient in Australia. Funct Ecol. 2001;15(2):222-232. https://doi.org/ 10.1046/j.1365-2435.2001.00508.x
  47. Prentice IC, Meng T, Wang H, Harrison P, Ni J, Wang G. Evidence of a universal scaling relationship for leaf CO 2 drawdown along an aridity gradient. New Phytol. 2011;190(1):169-180. https://doi.org/ 10.1111/j.1469-8137.2010.03579.x
  48. Ma F, Liang W, Zhou Z, et al. Spatial variation in leaf stable carbon isotope composition of three Caragana species in northern China. Forests. 2018;9(6):297. https://doi.org/10.3390/f9060297
  49. Körner C, Farquhar GD, Wong SC. Carbon isotope discrimination by plants follows latitudinal and altitudinal trends. Oecologia. 1991;88(1): 30-40.
  50. Wang N, Xu SS, Jia X, et al. Variations in foliar stable carbon isotopes among functional groups and along environmental gradients in China -a meta-analysis. Plant Biol. 2013;15(1):144-151. https://doi.org/10. 1111/j.1438-8677.2012.00605.x
  51. Ziegler S, Merker S, Streit B, Boner M, Jacob DE. Towards understanding isotope variability in elephant ivory to establish isotopic profiling and source-area determination. Biol Conserv. 2016;197:154-163.
  52. Kabalika Z, Morrison TA, McGill RAR, et al. Tracking animal movements using biomarkers in tail hairs: A novel approach for animal geolocating from sulfur isoscapes. Movement Ecol. 2020;8(1):37. https://doi.org/10.1186/s40462-020-00222-w
  53. Zazzo A, Monahan FJ, Moloney AP, Green S, Schmidt O. Sulphur isotopes in animal hair track distance to sea. Rapid Commun Mass Spectrom. 2011;25(17):2371-2378. https://doi.org/10.1002/rcm.5131
  54. Chukhrov FV, Ermilova LP, Churikov VS, Nosik LP. The isotopic composition of plant sulfur. Org Geochem. 1980;2(2):69-75. https:// doi.org/10.1016/0146-6380(80)90022-4
  55. Rees CE, Jenkins WJ, Monster J. The sulphur isotopic composition of ocean water sulphate. Geochim Cosmochim Acta. 1978;42(4):315-381. https://doi.org/10.1016/0016-7037(78)90268-5
  56. Trust BA, Fry B. Stable sulphur isotopes in plants: A review. Plant Cell Environ. 1992;15(9):1105-1110. https://doi.org/10.1111/j.1365- 3040.1992.tb01661.x
  57. Peterson BJ, Fry B. Stable isotopes in ecosystem studies. Annu Rev Ecol Syst. 1987;18(1):293-320.
  58. Webb EC, Newton J, Lewis J, et al. Sulphur-isotope compositions of pig tissues from a controlled feeding study. STAR: Sci Technol Archaeol Res. 2017;3(1):71-79. https://doi.org/10.1080/20548923.2017.1368821
  59. Peterson BJ, Howarth RW. Sulfur, carbon, and nitrogen isotopes used to trace organic matter flow in the salt-marsh estuaries of Sapelo Island, Georgia. Limnol Oceanogr. 1987;32(6):1195-1213. https://doi. org/10.4319/lo.1987.32.6.1195

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Background: Information on larval diet of many holometabolous insects remains incomplete. Carbon (C) and nitrogen (N) stable isotope analysis in adult wing tissue can provide an efficient tool to infer such trophic relationships. The present study examines whether moth feeding guild affiliations taken from literature are reflected in isotopic signatures. Results: Non-metric multidimensional scaling and permutational analysis of variance indicate that centroids of dietary groups differ significantly. In particular, species whose larvae feed on mosses or aquatic plants deviated from those that consumed vascular land plants. Moth δ 15 N signatures spanned a broader range, and were less dependent on species identity than δ 13 C values. Comparison between moth samples and ostensible food sources revealed heterogeneity in the lichenivorous guild, indicating only Lithosia quadra as an obligate lichen feeder. Among root-feeding Agrotis segetum, some specimens appear to have developed on crop plants in forest-adjacent farm land. Reed-feeding stem-borers may partially rely on intermediary trophic levels such as fungal or bacterial growth. Conclusion: Diagnostic partitioning of moth dietary guilds based on isotopic signatures alone could not be achieved, but hypotheses on trophic relationships based on often vague literature records could be assessed with high resolution. Hence, the approach is well suited for basic categorization of moths where diet is unknown or notoriously difficult to observe (i.e. Microlepidoptera, lichen-feeders).

Towards incorporating insect isotope analysis using cavity ring-down spectroscopy into area-wide insect pest management programs

Measurement of natural stable isotope signatures of insects has proven to be a useful method in determining their natal origin, feeding strategies and mating behavior, and has spawned a new discipline of insect isotope forensics. However the complexity of measuring isotope signatures using elemental analysis-isotope ratio mass-spectrometry (EA-IRMS) has encountered significant technical barriers, which together with costs, have hindered the advancement and wide spread adoption of this potentially useful approach. In the last decade simpler technologies to measure stable isotope ratios in samples based on laser spectroscopy have been developed. We foresee that these instruments will fuel the advancement and adoption of insect isotope forensics into pest management programs because they are easy to use, more affordable, and complement existing marking tools. However prior to the adoption of these new technologies it is necessary to test their fitness for purpose and explore their limitations. In this paper we set out to test the suitability of using combustion module-cavity ring-down spectroscopy (CM-CRDS) for measuring isotope ratios in an entomo-logical context, covering marking of insects, mating behavior and dietary assessment. We carried out a series of experiments to compare the isotope measurements made with the CM-CRDS with the traditional method of EA-IRMS. Initially we compared measurements of carbon isotope values of a variety of common diet components used in insect rearing, which covered a wide range of carbon isotope values. There was good agreement in the isotope values obtained, using the CM-CRDS and the EA-IRMS with similar accuracy and precision. Secondly we compared the 2 methods to measure carbon isotope values of the common cutworm, Spodoptera litura (Fabricius) (Lepidoptera: Noctuidae) samples, and again there was good agreement in the values obtained. Thirdly we tested whether the CM-CRDS could be used to determine the paternity of spermataphores, based on the differential isotope signatures of the paternal and maternal moths, as a result of differences in their rearing diets. The CM-CRDS proved to be fit for the purpose of measuring isotope values in the spermataphores of common cutworm and suggested that the CM-CRDS technology would be suitable for these isotope based mating studies in moths if the spermatophores were of sufficient mass. Finally we explored a number of the issues surrounding CM-CRDS and isotope technologies in general, e.g., logistical considerations, economics of operation, sample size, etc. We conclude that CM-CRDS is a suitable instrument for measuring stable isotope carbon signatures in moths, and most probably other sufficiently large insects and that CM-CRDS could be easily used in both operational and research contexts. Resumen La medición de las firmas de isótopos estables naturales de los insectos ha demostrado ser un método útil para determinar su origen natal, estra-tegias de alimentación y su comportamiento de apareamiento y ha dado lugar a una nueva disciplina de la ciencia forense de isótopos de insectos. Sin embargo, la complejidad de la medición de las firmas isotópicas usando el análisis de espectrometría de masas de ratio elemental de isótopos (AEM-REI) se ha encontrado con obstáculos técnicos importantes, que junto con los costos, han obstaculizado el avance y la adopción generalizada de este enfoque potencialmente útil. En la última decada se han desarrollado tecnologías más simples para medir las proporciones de isótopos estables en muestras basadas en espectroscopia láser. Prevemos que estos instrumentos se alimentan el avance y la adopción del uso de forense de isótopos de insectos en los programas de manejo de plagas, ya que son fáciles de usar, menos costos, y complementan las herramientas para marcar ya existentes. Sin embargo, antes de la adopción de estas nuevas tecnologías es necesario probar su aptitud para el uso y explorar sus limitaciones. En este trabajo nos propusimos evaluar el apropiado del uso de la espectroscopia de combustión de cavidad de módulo de anillo-abajo (ECC-MAA) para medir el ratio de los isótopos en un contexto entomológica, incluyendo el marcar de los insectos, el comportamiento del apareamiento y la evaluación de la dieta. Realizamos una serie de experimentos para comparar las medidas de isótopos realizadas con la ECM-CAA con el método tradicional de AEM-REI. Inicialmente se compararon las medidas de los valores de los isótopos de carbono de una variedad de componentes comunes utilizados en la dieta en la cría de insectos, que cubría una amplia gama de valores de los isótopos de carbono. Hubo buen acuerdo en los valores de isótopos obtenido, utilizando el ECM-CAA y el AEM-REI con exactitud y precisión similar. En segundo lugar se compararon los 2 métodos para medir los valores

Isotopes and Trace Elements as Natal Origin Markers of Helicoverpa armigera – An Experimental Model for Biosecurity Pests

PLoS ONE, 2014

Protecting a nation's primary production sector and natural estate is heavily dependent on the ability to determine the risk presented by incursions of exotic insect species. Identifying the geographic origin of such biosecurity breaches can be crucial in determining this risk and directing the appropriate operational responses and eradication campaigns, as well as ascertaining incursion pathways. Reading natural abundance biogeochemical markers using mass spectrometry is a powerful tool for tracing ecological pathways as well as provenance determination of commercial products and items of forensic interest. However, application of these methods to trace insects has been underutilised to date and our understanding in this field is still in a phase of basic development. In addition, biogeochemical markers have never been considered in the atypical situation of a biosecurity incursion, where sample sizes are often small, and of unknown geographic origin and plant host. These constraints effectively confound the interpretation of the one or two isotope geolocation markers systems that are currently used, which are therefore unlikely to achieve the level of provenance resolution required in biosecurity interceptions. Here, a novel approach is taken to evaluate the potential for provenance resolution of insect samples through multiple biogeochemical markers. The international pest, Helicoverpa armigera, has been used as a model species to assess the validity of using naturally occurring d 2 H, 87 Sr/ 86 Sr, 207 Pb/ 206 Pb and 208 Pb/ 206 Pb isotope ratios and trace element concentration signatures from single moth specimens for regional assignment to natal origin. None of the biogeochemical markers selected were individually able to separate moths from the different experimental regions (150-3000 km apart). Conversely, using multivariate analysis, the region of origin was correctly identified for approximately 75% of individual H. armigera samples. The geographic resolution demonstrated with this approach has considerable potential for biosecurity as well as other disciplines including forensics, ecology and pest management.

Stable Isotope Markers Differentiate between Mass-Reared and Wild Lepidoptera in Sterile Insect Technique Programs

Florida Entomologist, 2016

In this study we identified a number of moth (Lepidoptera) species that are potential targets for the sterile insect technique (SIT), and we assessed the feasibility of using stable isotope signatures as markers to distinguish mass-reared from wild moth species. Large natural differences in the isotopic signatures of commercially available sugars render them novel markers for mass-reared insects. Sugar beet (Beta vulgaris L.; Caryophyllales: Amaranthaceae), a C 3 plant, has a stable isotopic signature (a measure of the ratio of the stable isotopes 13 C: 12 C) of around −27‰ relative to Vienna Pee Dee Belemnite (VPDB; the international C isotope standard for the stable isotopes, 13 C and 12 C), and sugarcane (Saccharum spp.; Poales: Poaceae), a C 4 plant, has an isotopic signature of around −11‰. Thus by means of such a distinct isotope ratio in the sugar in the diet, mass-reared insects can be easily distinguished from wild insects with a high degree of certainty. It was shown that the method could be extended using a multiple isotope approach, with 15 N or a full suite of C, N, S and O isotopes. Intrinsic isotope marking of mass-reared moths proved to be an accurate means of distinguishing wild from mass-reared populations, based on isotopic differences between the wild host plant species and the diets used in mass-rearing, which where possible, had been manipulated to contain the isotopically divergent sugar type. This intrinsic labeling using stable isotopes could be useful in the assessment of the quality of mass-reared moths, because a stable isotope is a marker that does not affect the insect in any detrimental manner.

Change in carbon stable isotope ratios of the predatory bug Orius majusculus after dietary shifts

Entomologia Experimentalis et Applicata, 2013

Orius majusculus Reuter (Hemiptera: Anthocoridae) is an important component of the pest predatory complex in arable crops in Mediterranean areas. It moves between crops searching for prey, and improving knowledge on its dispersal abilities will help to develop conservation biological control strategies. Stable isotope ratios may be used as a tool for tracking insect movements, as the isotopic composition of insect tissues changes to reflect that of their diet when they undergo dietary shifts on moving between isotopically distinct crops. We carried out laboratory diet switch experiments with a stable isotope approach to infer information on dispersal of O. majusculus individuals among C3 and C4 crops to better understand isotopic field data collections. Switching the aphid food source caused a quick change in d 13 C signatures, regardless of the original and final food source. Changes in the d 13 C ratio of O. majusculus after diet switching fitted with an exponential model that showed similar turnover rates, and thus half-lives, between shifting diets up to 20 days. Subsequently, whereas individuals feeding on C4 aphids did not survive, turnover rate decreased in individuals that switched from C4 to C3 aphids. However, d 13 C traces from the original source remained in the predator until 25 days after switching, and this is enough time to help determine the movement of O. majusculus between crops in the field and to plan the timing of predator sampling and crop practices that may enhance predator ecological services. Orius majusculus that switched to a maize aphid diet showed different turnover rates between sexes, although this did not influence the pattern of switchover.

Using light stable isotopes to understand nutrient cycling in soils and how these isotopic techniques can be leveraged to investigate the ecology and biology of insects – A review

Die Bodenkultur: Journal of Land Management, Food and Environment

Summary At first glance, there appears little to link nitrogen cycling with entomology other that the use of isotope techniques. Soil management requires a contextual, adaptive, flexible approach that is based on understanding the factors that regulate the soil’s fundamental processes. Using stable isotope techniques for the analysis of the inherent biogeochemical processes can explain the complex soil–plant interactions, the determining factors of the nitrogen cycle, and the impacts of applying external inputs. Using the same stable isotope tools enables an interdisciplinary collaboration between soil science and entomology. Emerging plant pests, for instance, non-native insect species, are a threat to the agroecosystems. The knowledge of the origin and movement of invasive insects by using the intrinsic stable isotope signatures embedded in the environment allows identification of entry pathways and thus the establishment of effective management strategies to reduce the potential ...

Using stable isotopes to trace long-distance dispersal in birds and other taxa

Diversity and Distributions, 2005

Hydrogen isotopes reveal evidence of migration of Miniopterus schreibersii in Europe

BMC Ecology

Background The Schreiber’s bat, Miniopterus schreibersii, is adapted to long-distance flight, yet long distance movements have only been recorded sporadically using capture-mark-recapture. In this study, we used the hydrogen isotopic composition of 208 wing and 335 fur specimens from across the species' European range to test the hypothesis that the species migrates over long distances. Results After obtaining the hydrogen isotopic composition (δ2H) of each sample, we performed geographic assignment tests by comparing the δ2H of samples with the δ2H of sampling sites. We found that 95 bats out of 325 showed evidence of long-distance movement, based on the analysis of either fur or wing samples. The eastern European part of the species range (Greece, Bulgaria and Serbia) had the highest numbers of bats that had moved. The assignment tests also helped identify possible migratory routes, such as movement between the Alps and the Balkans. Conclusions This is the first continental-sc...

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    Autumn migration of the migrant hawker (Aeshna mixta) at the Baltic coast

    Movement Ecology

    Background Migratory insects are important for the provision of ecosystem services both at the origin and destination sites but – apart from some iconic species – the migration routes of many insect species have not been assessed. Coastlines serve as a funnel where migrating animals including insects accumulate. Migratory behaviour and captures of dragonflies in bird traps suggest autumn migration of dragonflies along coastlines while the origin and regularity of this migration remain unclear. Methods Dragonfly species were caught at the bird observatory Kabli at the Baltic coast in Estonia in 2009, 2010 and 2015. For the 2015 data set, we used a stable hydrogen (H) approach to trace the potential natal origin of the migrant hawker (Aeshna mixta). Results 1079 (2009), 701 (2010) and 88 (2015) A. mixta individuals were caught during the study periods (35, 37 and 11 days in 2009, 2010 and 2015, respectively). The migration period lasted from end of August to end of September. Based on...

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