47 citations as recorded by crossref.

1. Selective stabilization of soil fatty acids related to their carbon chain length and presence of double bonds in the Peruvian Andes S. Yang et al. 10.1016/j.geoderma.2020.114414
2. Discharge‐Modulated Soil Organic Carbon Export From Temperate Mountainous Headwater Streams H. Gies et al. 10.1029/2021JG006624
3. Development of a QuEChERS-based method combined with gas chromatography-mass spectrometry for the analysis of alkanes in sediments A. Herrera-Herrera et al. 10.1016/j.microc.2020.104774
4. Molecular and isotopic biogeochemistry on recently-formed soils on King George Island (Maritime Antarctica) after glacier retreat upon warming climate S. Vega-García et al. 10.1016/j.scitotenv.2020.142662
5. Warming and elevated CO2 promote rapid incorporation and degradation of plant‐derived organic matter in an ombrotrophic peatland N. Ofiti et al. 10.1111/gcb.15955
6. Severe drought-influenced composition and δ13C of plant and soil n-alkanes in model temperate grassland and heathland ecosystems K. Srivastava & G. Wiesenberg 10.1016/j.orggeochem.2017.11.002
7. Biomarker fatty acids of permafrost peat plateaus of the Komi Republic E. Lyu-Lyan-Min & I. Gruzdev 10.1088/1755-1315/862/1/012059
8. Modelling leaf wax n -alkane inputs to soils along a latitudinal transect across Australia S. Howard et al. 10.1016/j.orggeochem.2018.03.013
9. Asthma-protective agents in dust from traditional farm environments M. Marques dos Santos et al. 10.1016/j.jaci.2023.05.013
10. Impact of weathering processes on n-alkane pattern in badlands M. Stefanović et al. 10.1016/j.catena.2023.107352
11. Afforestation Alters the Molecular Composition of Soil Organic Matter in the Central Loess Plateau of China X. Song et al. 10.3390/f14071502
12. Soil organic carbon content and mineralization controlled by the composition, origin and molecular diversity of organic matter: A study in tropical alpine grasslands S. Yang et al. 10.1016/j.still.2021.105203
13. Catchment-wide variations and biogeochemical time lags in soil fatty acid carbon isotope composition for different land uses: Implications for sediment source classification H. Upadhayay et al. 10.1016/j.orggeochem.2020.104048
14. Wax lipids in fresh and charred anatomical parts of the Celtis australis tree: Insights on paleofire interpretation M. Jambrina-Enríquez et al. 10.1016/j.orggeochem.2018.05.017
15. Transformation of <i>n</i>-alkanes from plant to soil: a review C. Thomas et al. 10.5194/soil-7-785-2021
16. Organic matter biomarker and 13C NMR characteristics of soil and sediment standard reference materials from China G. Sun et al. 10.1016/j.scitotenv.2022.155661
17. Tree species richness and N-fixing tree species enhance the chemical stability of soil organic carbon in subtropical plantations X. Ye et al. 10.1016/j.soilbio.2022.108828
18. Quantification of lipid biomarkers in sedimentary contexts: Comparing different calibration methods A. Herrera-Herrera & C. Mallol 10.1016/j.orggeochem.2018.07.009
19. Compound-specific isotope analysis with nested sampling approach detects spatial and temporal variability in the sources of suspended sediments in a Scottish mesoscale catchment P. Hirave et al. 10.1016/j.scitotenv.2020.142916
20. Characteristic of Molecular Weight-Fractions of Soil Organic Matter from Calcareous Soil and Yellow Soil L. Ma & B. Xiao 10.3390/su15021537
21. Epicuticular wax lipid composition of endemic European Betula species in a simulated ontogenetic/diagenetic continuum and its application to chemotaxonomy and paleobotany J. Weber & L. Schwark 10.1016/j.scitotenv.2020.138324
22. Leaf wax n-alkanes in leaves, litter, and surface soil in a low diversity, temperate deciduous angiosperm forest, Central Missouri, USA S. Stout 10.1080/02757540.2020.1789118
23. Chemical characterization of mountain forest soils: impact of long-term atmospheric deposition loadings (Czech–Polish–German border region) M. Havelcová et al. 10.1007/s11356-020-08558-x
24. Characterization and chemo-taxonomic evaluation of plant leaf waxes (long chain n-alkanoic acids, n-alkanes and n-alkanols) as a vegetation biomarker from species of the South American temperate forest (STF) C. Cerda-Peña & S. Contreras 10.1016/j.ecolind.2022.108675
25. Prolonged heavy rainfall and land use drive catchment sediment source dynamics: Appraisal using multiple biotracers H. Upadhayay et al. 10.1016/j.watres.2022.118348
26. Late-season biosynthesis of leaf fatty acids and n-alkanes of a mature beech (Fagus sylvatica) tree traced via13CO2 pulse-chase labelling and compound-specific isotope analysis T. Speckert et al. 10.3389/fpls.2022.1029026
27. n-Alkanes and their carbon isotopes (δ13C) reveal seasonal foddering and long-term corralling of pastoralist livestock in eastern Mongolia N. Égüez et al. 10.1016/j.jas.2022.105666
28. From leaf to soil: <i>n</i>-alkane signal preservation, despite degradation along an environmental gradient in the tropical Andes M. Teunissen van Manen et al. 10.5194/bg-17-5465-2020
29. Middle Bronze Age land use practices in the northwestern Alpine foreland – a multi-proxy study of colluvial deposits, archaeological features and peat bogs S. Scherer et al. 10.5194/soil-7-269-2021
30. Preserved lipid signatures in palaeosols help to distinguish the impacts of palaeoclimate and indigenous peoples on palaeovegetation in northwest Siberia L. Harrault et al. 10.1016/j.orggeochem.2022.104407
31. Distribution of n-alkanes and their δ2H and δ13C values in typical plants along a terrestrial-coastal-oceanic gradient D. He et al. 10.1016/j.gca.2020.05.003
32. Soil Perturbation in Mediterranean Ecosystems Reflected by Differences in Free-Lipid Biomarker Assemblages P. Tinoco et al. 10.1021/acs.jafc.8b01483
33. Land-use-based freshwater sediment source fingerprinting using hydrogen isotope compositions of long-chain fatty acids P. Hirave et al. 10.1016/j.scitotenv.2023.162638
34. Variation in leaf wax n-alkane characteristics with climate in the broad-leaved paperbark (Melaleuca quinquenervia) J. Andrae et al. 10.1016/j.orggeochem.2019.02.004
35. Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter N. Ofiti et al. 10.1016/j.soilbio.2021.108185
36. Livestock activity biomarkers: Estimating domestication and diet of livestock in ancient samples C. Vázquez et al. 10.1016/j.jasrep.2021.103220
37. The Biological Origins of Soil Organic Matter in Different Land-Uses in the Highlands of Ethiopia D. Assefa et al. 10.3390/f13040560
38. Sensitivity of source apportionment predicted by a Bayesian tracer mixing model to the inclusion of a sediment connectivity index as an informative prior: Illustration using the Kharka catchment (Nepal) H. Upadhayay et al. 10.1016/j.scitotenv.2020.136703
39. Novel sediment source fingerprinting quantifying erosion-induced total nitrogen and total phosphorus outputs from an intensive agricultural catchment, North China H. Yu et al. 10.1016/j.iswcr.2022.10.006
40. Carbon and hydrogen isotopes of taraxerol in mangrove leaves and sediment cores: Implications for paleo-reconstructions D. He et al. 10.1016/j.gca.2022.02.018
41. Soil carbon storage predicted from the diversity of pyrolytic alkanes M. Jiménez-González et al. 10.1007/s00374-018-1285-6
42. Leaf wax n‐alkane patterns of six tropical montane tree species show species‐specific environmental response M. Teunissen van Manen et al. 10.1002/ece3.5458
43. Understanding the effects of early degradation on isotopic tracers: implications for sediment source attribution using compound-specific isotope analysis (CSIA) P. Hirave et al. 10.5194/bg-17-2169-2020
44. Turnover of non-polymeric leaf lipids in a loamy grassland soil C. Warren & O. Butler 10.1007/s11104-023-06027-1
45. Origin, transport, and retention of fluvial sedimentary organic matter in South Africa's largest freshwater wetland, Mkhuze Wetland System J. Gensel et al. 10.5194/bg-19-2881-2022
46. Petroleum contamination evaluation and bacterial community distribution in a historic oilfield located in loess plateau in China S. Gao et al. 10.1016/j.apsoil.2018.12.012
47. Abundance of lipids in differently sized aggregates depends on their chemical composition G. Angst et al. 10.1007/s10533-018-0481-7