124 citations as recorded by crossref.

1. Reconstructing Mid-Pleistocene paleovegetation and paleoclimate in the Golan Heights using the δ13C values of modern vegetation and soil organic carbon of paleosols G. Hartman 10.1016/j.jhevol.2010.08.001
2. Sources and features of particulate organic matter in tropical small mountainous rivers (SW China) under the effects of anthropogenic activities Y. Zhang et al. 10.1016/j.ecolind.2021.107471
3. Mangrove forest degradation indicated by mangrove-derived organic matter in the Qinzhou Bay, Guangxi, China, and its response to the Asian monsoon during the Holocene climatic optimum X. Meng et al. 10.1007/s13131-015-0778-5
4. Altered cropping pattern and cultural continuation with declined prosperity following abrupt and extreme arid event at ~4,200 yrs BP: Evidence from an Indus archaeological site Khirsara, Gujarat, western India A. Pokharia et al. 10.1371/journal.pone.0185684
5. Organic Carbon Storage and 14C Apparent Age of Upland and Riparian Soils in a Montane Subtropical Moist Forest of Southwestern China X. Liu et al. 10.3390/f11060645
6. Foliar δ13C Showed No Altitudinal Trend in an Arid Region and Atmospheric Pressure Exerted a Negative Effect on Plant δ13C Z. Chen et al. 10.3389/fpls.2017.01070
7. Organic matter transformation in the peat column at Marcell Experimental Forest: Humification and vertical stratification M. Tfaily et al. 10.1002/2013JG002492
8. Climatic significance of the stable carbon isotopic composition of surface soils in northern Iran and its application to an Early Pleistocene loess section Q. Wang et al. 10.1016/j.orggeochem.2018.11.011
9. Determination of the geographic origin of garlic using the bioelement content and isotope signatures S. Choi et al. 10.1016/j.foodcont.2021.108339
10. Glacial-interglacial vegetation changes in northeast China inferred from isotopic composition of pyrogenic carbon from Lake Xingkai sediments W. Sun et al. 10.1016/j.orggeochem.2018.03.004
11. Palaeochannels of Australia's Riverine Plain - Reconstructing past vegetation environments across the Late Pleistocene and Holocene M. Forbes et al. 10.1016/j.palaeo.2019.109533
12. New sedimentary evidence reveals a unique history of C4 biomass in continental East Asia since the early Miocene B. Zhou et al. 10.1038/s41598-017-00285-7
13. Peat δ13Ccelluose-recorded wetting trend during the past 8000 years in the southern Altai Mountains, northern Xinjiang, NW China D. Zhang et al. 10.1016/j.jseaes.2018.01.029
14. New climatic oscillations during MIS 11c in the record of the Skrzynka II site (Eastern Poland) based on palynological and isotope analysis A. Górecki et al. 10.1016/j.quaint.2021.09.017
15. Climate and CO<sub>2</sub> modulate the C<sub>3</sub>/C<sub>4</sub> balance and δ<sup>13</sup>C signal in simulated vegetation O. Flores et al. 10.5194/cp-5-431-2009
16. Organic carbon isotope and molecular fossil records of vegetation evolution in central Loess Plateau since 450 kyr B. Zhou et al. 10.1007/s11430-016-5276-x
17. Local variation in climate and land use during the time of the major kingdoms of the Tigray Plateau in Ethiopia and Eritrea V. Terwilliger et al. 10.1016/j.catena.2010.08.003
18. Holocene land cover change in south-western Amazonia inferred from paleoflood archives U. Lombardo et al. 10.1016/j.gloplacha.2019.01.008
19. Spatial and temporal variations of C3/C4 relative abundance in global terrestrial ecosystem since the Last Glacial and its possible driving mechanisms Z. Rao et al. 10.1007/s11434-012-5233-9
20. Trend of increasing Holocene summer precipitation in arid central Asia: Evidence from an organic carbon isotopic record from the LJW10 loess section in Xinjiang, NW China H. Xie et al. 10.1016/j.palaeo.2018.04.006
21. Variations of the Indian summer monsoon over the last 30 000 years inferred from a pyrogenic carbon record from south‐west China E. Zhang et al. 10.1002/jqs.3008
22. Carbon concentration and isotope composition of black carbon in the topsoil of the central and southeastern Qinghai-Tibetan Plateau, and their environmental significance L. Liu et al. 10.1016/j.catena.2018.08.011
23. Variations in carbon isotope ratios of plants across a temperature gradient along the 400 mm isoline of mean annual precipitation in north China and their relevance to paleovegetation reconstruction G. Wang et al. 10.1016/j.quascirev.2012.12.004
24. Effects of environmental and biotic factors on carbon isotopic fractionation during decomposition of soil organic matter G. Wang et al. 10.1038/srep11043
25. Effect of burning on the distribution pattern and isotopic composition of plant biomolecules: Implications for paleoecological studies V. Sarangi et al. 10.1016/j.gca.2021.12.003
26. Climatic control on the C3 and C4 plant abundance during the late Pleistocene – Holocene in the northern Gangetic Plain, India M. Kumar et al. 10.1016/j.palaeo.2022.110890
27. Hominin Response to Oscillations in Climate and Local Environments During the Mid‐Pleistocene Climate Transition in Northern China B. Zhou et al. 10.1029/2023GL104931
28. Variation in carbon isotopic composition over the past ca. 46,000yr in the loess–paleosol sequence in central Kazakhstan and paleoclimatic significance M. Ran & Z. Feng 10.1016/j.orggeochem.2014.05.006
29. Agricultural resilience and land-use from an Indus settlement in north-western India: Inferences from stable Carbon and Nitrogen isotopes of archaeobotanical remains S. Sharma et al. 10.1007/s12520-024-01971-0
30. Effect of salinity on the preservation of plant-derived n-alkyl compounds in the terrestrial-aquatic interface S. Samantaray & P. Sanyal 10.1016/j.orggeochem.2023.104653
31. Is it C4 or ‘C3 in disguise’? Disentangling the ambiguity in palaeovegetation estimation A. SREEMANY & M. BERA 10.1002/jqs.3427
32. The key factor limiting plant growth in cold and humid alpine areas also plays a dominant role in plant carbon isotope discrimination M. Xu et al. 10.3389/fpls.2015.00961
33. Altitudinal trends of leaf δ13C follow different patterns across a mountainous terrain in north China characterized by a temperate semi‐humid climate G. Wang et al. 10.1002/rcm.4543
34. The respective characteristics of millennial-scale changes of the India summer monsoon in the Holocene and the Last Glacial B. Hong et al. 10.1016/j.palaeo.2018.01.033
35. Seasonality of C4 plant growth and carbonate precipitation in the Chinese Loess Plateau may cause positive carbon isotope anomalies in pedogenic carbonates Y. Fu et al. 10.1017/qua.2023.66
36. Variations in carbon isotope ratios of C3 plants and distribution of C4 plants along an altitudinal transect on the eastern slope of Mount Gongga J. Li et al. 10.1007/s11430-009-0170-4
37. Nitrogen isotopes suggest a change in nitrogen dynamics between the Late Pleistocene and modern time in Yukon, Canada F. Tahmasebi et al. 10.1371/journal.pone.0192713
38. Nitrogen and carbon isotopic dynamics of subarctic soils and plants in southern Yukon Territory and its implications for paleoecological and paleodietary studies F. Tahmasebi et al. 10.1371/journal.pone.0183016
39. Using δ13C to reveal the importance of different water transport pathways in two nested karst basins, Southwest China Z. Hao et al. 10.1016/j.jhydrol.2019.01.070
40. Response of Travertine Dam to Precipitation over the Past 800 Years in Zabuye Salt Lake, Southwestern Tibetan Plateau M. Li et al. 10.3390/min12070916
41. Response of arid northeast Mexico to global climate changes during the late Pleistocene to the middle Holocene P. Roy et al. 10.1002/esp.4645
42. Speculation for quantifying increased C4 plants under future climate conditions: Inner Mongolia, China case study X. Ma et al. 10.1016/j.quaint.2021.03.011
43. Carbon isotope variations of modern soils in the eastern margin of the Tibetan Plateau and their controlling factors L. Qi et al. 10.1007/s11629-019-5863-3
44. Stable carbon isotopic composition of black carbon in surface soil as a proxy for reconstructing vegetation on the Chinese Loess Plateau L. Liu et al. 10.1016/j.palaeo.2013.08.012
45. Temperate coastal wetland near-surface carbon storage: Spatial patterns and variability C. Owers et al. 10.1016/j.ecss.2020.106584
46. Alternation between terrestrial and aquatic plants dominated organic matter sources in the Tiaoshu wetland (south China) and its response to late Pleistocene environmental changes J. Chen et al. 10.1016/j.palaeo.2024.112168
47. Peat humification- and δ13Ccellulose-recorded warm-season moisture variations during the past 500 years in the southern Altai Mountains within northern Xinjiang of China D. Zhang et al. 10.1007/s11629-017-4538-1
48. Stable carbon analysis of alluvial paleosols in the Mixteca Alta, Oaxaca, Mexico G. Holdridge & D. Leigh 10.1016/j.quaint.2018.05.020
49. C4 expansion of Central Asia in the middle Miocene linked to the strengthening Indian monsoon J. Wang et al. 10.1016/j.gloplacha.2023.104096
50. In-situ 13CO2 labeling to trace carbon fluxes in plant-soil-microorganism systems: Review and methodological guideline R. Pang et al. 10.1016/j.rhisph.2021.100441
51. δ13C values of plants as indicators of soil water content in modern ecosystems of the Chinese Loess Plateau J. Wei et al. 10.1016/j.ecoleng.2015.01.012
52. Distribution and carbon isotopic composition of long-chain leaf wax n-alkanes from Holocene lake sediments in the Altai Mountains Q. Li et al. 10.1016/j.quaint.2022.04.008
53. Last 10 millennial history of Indian summer monsoon in the Bengal region – a multi-proxy reconstruction from a lacustrine archive R. Ghosh et al. 10.1016/j.palaeo.2022.111308
54. Landscape evolution of the Ganga-Sai interfluve in response to river dynamics and Late Pleistocene-Holocene climate change via a meander cut-off lake of a plains-fed channel P. Misra et al. 10.1016/j.geomorph.2024.109068
55. Ancient origin of a rainforest in Gabon as revealed by carbon isotope data of vegetation and soil S. Pietsch & S. Gautam 10.1177/0959683613505341
56. A Negative Relationship between Foliar Carbon Isotope Composition and Mass-Based Nitrogen Concentration on the Eastern Slope of Mount Gongga, China J. Li et al. 10.1371/journal.pone.0166958
57. Variation and paleoclimatic significance of organic carbon isotopes of Ili loess in arid Central Asia Z. Rao et al. 10.1016/j.orggeochem.2013.08.007
58. A Younger Dryas signature in bison bone stable isotopes from the southern Plains of North America K. Carlson et al. 10.1016/j.jasrep.2017.03.001
59. Dynamics of organic matter in soils formed on limestone and sandstone in the karst area in southwestern China: δ 13C and δ 15N approaches L. Li et al. 10.1088/1755-1315/861/6/062046
60. Variation of surface soil δ13Corg in the upper and middle reaches of the Yarlung Zangbo river basin, southern Tibetan Plateau, and its climatic implications S. Wang et al. 10.1016/j.sedgeo.2022.106135
61. Anti-phase oscillation of Asian monsoons during the Younger Dryas period: Evidence from peat cellulose δ13C of Hani, Northeast China B. Hong et al. 10.1016/j.palaeo.2010.08.004
62. Climatic significance of modern minute land snail shells δ13C and δ18O on the Chinese Loess Plateau X. Zong et al. 10.1016/j.ecolind.2022.109733
63. Stable carbon isotope of black carbon in lake sediments as an indicator of terrestrial environmental changes: An evaluation on paleorecord from Daihai Lake, Inner Mongolia, China X. Wang et al. 10.1016/j.chemgeo.2013.03.009
64. Fire history of the Chinese Loess Plateau under extreme warming scenarios: A case study of the loess-paleosol sequence L5-S5 L. Liu & S. Yang 10.1016/j.quaint.2020.09.031
65. The disparity in the abundance of C4 plants estimated using the carbon isotopic composition of paleosol components V. Sarangi et al. 10.1016/j.palaeo.2020.110068
66. Soil organic matter dynamics under different land use in grasslands in Inner Mongolia (northern China) L. Zhao et al. 10.5194/bg-11-5103-2014
67. Summer moisture changes in the Lake Qinghai area on the northeastern Tibetan Plateau recorded from a meadow section over the past 8400 yrs X. Li et al. 10.1016/j.gloplacha.2017.11.016
68. Response to palaeoclimate by Early Cretaceous terrestrial organic-rich shales in the Yin'e Basin: Evidence from sporopollen, n-alkanes and their compound carbon isotopes G. Liu et al. 10.1016/j.palaeo.2024.112031
69. The challenge of the unique and unprecedented, comment on Agnihorti et al. (2021) J. Bates et al. 10.1016/j.jasrep.2021.103174
70. Chemical and carbon isotopic dynamics of grass organic matter during litter decompositions: A litterbag experiment G. Wang et al. 10.1016/j.orggeochem.2014.02.012
71. The precipitation “threshold value” on C4/C3 abundance of the Loess Plateau, China B. Sun et al. 10.1007/s11434-014-0675-x
72. Soil carbon isotope ratios of the Zijing site, Qinling Mountains, China: Implications for defining the southern limit of millet agriculture P. Zhang et al. 10.1016/j.quaint.2013.01.003
73. Evaluating the response of <i>δ</i><sup>13</sup>C in <i>Haloxylon ammodendron</i>, a dominant C<sub>4</sub> species in Asian desert ecosystems, to water and nitrogen addition as well as the availability of its <i>δ</i><sup>13</sup>C as an indicator of water use efficiency Z. Chen et al. 10.5194/bg-18-2859-2021
74. Comments on “Anti-phase oscillation of Asian monsoons during the Younger Dryas period: Evidence from peat cellulose δ13C of Hani, Northeast China” by B. Hong, Y.T. Hong, Q.H. Lin, Yasuyuki Shibata, Masao Uchida, Y.X. Zhu, X.T. Leng, Y. Wang and C.C. Cai [Palaeogeography, Palaeoclimatology, Palaeoecology 297 (2010) 214–222] M. Stebich et al. 10.1016/j.palaeo.2011.06.004
75. Transportation characteristics of δ 13C in the plants-soil-bedrock-cave system in Chongqing karst area T. Li et al. 10.1007/s11430-011-4294-y
76. Relationship between stable carbon and nitrogen isotope ratios of humic acids extracted from Andisols and non-Andisols N. Katsumi et al. 10.1016/j.catena.2015.01.005
77. n-Alkanes and compound carbon isotope records from Lake Yiheshariwusu in the Hulun Buir sandy land, northeastern China M. Xie et al. 10.1177/0959683620932968
78. Addressing the Relationship between Leaf Nitrogen and Carbon Isotope Discrimination from the Three Levels of Community, Population and Individual S. Wang et al. 10.3390/plants12071551
79. Temperature exerts no influence on organic matter <i>δ</i><sup>13</sup>C of surface soil along the 400 mm isopleth of mean annual precipitation in China Y. Jia et al. 10.5194/bg-13-5057-2016
80. The potential of contribution of mangrove-derived organic matter in intertidal sediments as a proxy of mangrove development in the northern Beibu Gulf J. Zhang et al. 10.1007/s13131-020-1640-y
81. Plant-wax carbon isotopic evidence of Lateglacial and Holocene climate change from lake sediments in the Yin Mountains, inner Mongolia H. Dong et al. 10.1016/j.quaint.2021.12.017
82. Influence of provenance and preservation on the carbon isotope variations of dispersed organic matter in ancient floodplain sediments C. Bataille et al. 10.1002/ggge.20294
83. Effects of climate factors on spatiotemporal variation in carbon and oxygen isotope ratios in Korean rice S. Choi et al. 10.1016/j.jfca.2022.104416
84. Disentangling temperature effects on leaf wax n-alkane traits and carbon isotopic composition from phylogeny and precipitation J. Wang et al. 10.1016/j.orggeochem.2018.10.008
85. Black carbon concentration and isotopic composition of surface sand from deserts and dune fields in Northern China L. Liu et al. 10.1016/j.palaeo.2015.12.026
86. Stable Carbon Isotopic Composition of Black Carbon in Surface Soil as a Proxy for Reconstructing Vegetation on the Northern Slope of the Qinling Mountains L. Lian et al. 10.1111/1755-6724.12653
87. Precipitation reconstruction since the last deglacial based on the stable carbon isotopic composition of a loess section in western Central Asia D. Zhang et al. 10.1177/09596836221126134
88. Mangrove Development and Its Response to Asian Monsoon in the Yingluo Bay (SW China) over the Last 2000 years X. Meng et al. 10.1007/s12237-016-0156-3
89. Carbon and nitrogen stable isotope ratios of soils and grasses as indicators of soil characteristics and biological taxa I. Shtangeeva et al. 10.1016/j.apgeochem.2019.03.009
90. A Persistently Increasing Precipitation Trend Through the Holocene in Northwest China Recorded by Black Carbon δ13C From Sayram Lake Q. Jiang et al. 10.3389/feart.2020.00228
91. Continuous measurements in North China and culture experiments reveal the potential of leaf n-alkane carbon isotopes in paleoclimate studies M. Shi et al. 10.1016/j.gloplacha.2023.104206
92. Relationship Between C4Biomass and C4Agriculture During the Holocene and its Implications for Millet Domestication in Northeast China J. Wang et al. 10.1029/2020GL089566
93. 100 k.y. pacing of the East Asian summer monsoon over the past five glacial cycles inferred from land snails R. Bao et al. 10.1130/G50243.1
94. Reconstruction of Late Glacial and Holocene landscape-climatic changes in the central Selenga Middle Mountains based on the isotopic composition of organic matter V. Golubtsov & Y. Ryzhov 10.1134/S106422931702003X
95. Stable carbon isotope records of black carbon on Chinese Loess Plateau since last glacial maximum: An evaluation on their usefulness for paleorainfall and paleovegetation reconstruction X. Wang et al. 10.1016/j.palaeo.2017.08.008
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98. Mangrove degradation and response to anthropogenic disturbance in the Maowei Sea (SW China) since 1926 AD: Mangrove-derived OM and pollen X. Meng et al. 10.1016/j.orggeochem.2016.06.001
99. Soil aggregate fraction-based 14C analysis and its application in the study of soil organic carbon turnover under forests of different ages W. Tan et al. 10.1007/s11434-012-5660-7
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102. Vegetation dynamics during the Pleistocene–Holocene transition in the central Great Plains, USA T. Woodburn et al. 10.1177/0959683616652710
103. Stable Carbon and Oxygen Isotopes in Shell Carbonates of modern Land Snails in China and Their Relation to Environment Variables X. Wang et al. 10.1029/2019JG005255
104. Increased winter-spring precipitation from the last glaciation to the Holocene inferred from a δ13Corg record from Yili Basin (Xinjiang, NW China) K. Zhao et al. 10.1007/s11430-018-9333-x
105. Characteristics and Sources of Black Carbon and Organic Carbon in Topsoil from Different Functional Zones of Beijing, China L. Liu & S. Yang 10.1134/S1064229321060090
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113. Consistent C3 plant habitat of hominins during 400–300 ka at the Longyadong Cave site (Luonan Basin, central China) revealed by stable carbon isotope analyses of loess deposits H. Zhang et al. 10.1016/j.jhevol.2017.01.011
114. Vegetation variation of loess deposits in the southeastern Inner Mongolia, NE China over the past ∼1.08 million years A. Lyu et al. 10.1016/j.jseaes.2017.11.013
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118. Evolution of the relative abundance of C4 plants on the Chinese Loess Plateau since the Last Glacial Maximum and its implications W. Jiang et al. 10.1002/jqs.3084
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123. Spatiotemporal changes in C4 plant abundance in China since the Last Glacial Maximum and their driving factors W. Jiang et al. 10.1016/j.palaeo.2018.12.021
124. Variations of surface soil δ13Corg in the different climatic regions of China and paleoclimatic implication D. Zhang et al. 10.1016/j.quaint.2019.12.015