1. Hebei Key Laboratory of Environmental Change and Ecological Construction, College of Geographical Sciences, Hebei Normal University, Shijiazhuang 050024, China 2. Hebei Center for Ecological and Environmental Geology Research, Hebei GEO University, Shijiazhuang 050031, China
The layers of Tamarix cones within sedimentary deposits in arid regions have significant chronological and paleoenvironmental implications. Here, we compare the δ18O values of Tamarix cones in the Hongliujing area of Lop Nur with meteorological data for the Ruoqiang meteorological station for 1960–2019 AD. Linear regression analysis was used to reconstruct the average temperature for April and the precipitation for November in the Hongliujing area over the past 200 years. The results showed that the δ18O values were significantly negatively correlated with the temperature for February, April, May, August, December, and with the annual mean temperature; significantly negatively correlated with the precipitation for February and April; significantly negatively correlated with the sunshine hours for March and May; significantly positively correlated with the sunshine hours for February, July, August, October, and December, and with the annual mean values; and significantly correlated with the relative humidity for April, July, August, September, October, and November, and with the annual mean values. Based on the δ18O record of the past 200 years, the Hongliujing area experienced two warm-wet periods (1874–1932 and 2004–2019 AD) and two cold-dry periods (1832–1873 and 1933–2003 AD). Thus, the climate was characterized by alternating warm-wet and cold-dry conditions. Wavelet analysis revealed three main cycles: 45 years, 29 years, and 14 years.
. [J]. Frontiers of Earth Science, 2023, 17(4): 970-980.
Zhiguang LI, Yaqing DONG, Haoyu ZHANG, Hongxiao SUN, Danyang JIA, Shikai SONG, Yuanjie ZHAO. Climate change in the Hongliujing area of Lop Nur over the past 200 years revealed by the stable oxygen isotopes of Tamarix cones. Front. Earth Sci., 2023, 17(4): 970-980.
F, Chen J, Chen W, Huang S, Chen X, Huang L, Jin J, Jia X, Zhang C, An J, Zhang Y, Zhao Z, Yu R, Zhang J, Liu A, Zhou S Feng (2019). Westerlies Asia and monsoonal Asia: spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales.Earth Sci Rev, 192: 337–354 https://doi.org/10.1016/j.earscirev.2019.03.005
2
F, Chen H, Shang Y Yuan (2016). Comparative analysis between tree-ring based drought records of Populus euphratica and Picea schrenkiana from the mountains and plains of eastern Xinjiang.Desert and Oasis Meteorology, 10(01): 34–40 (in Chinese)
3
F, Chen Y, Yuan W, Wei S, Yu H, Shang T, Zhang R, Zhang H Wang (2017b). Air temperature from May through August in northern Xinjiang reconstructed from multi-site tree-ring density.J Glaciol Geocryol, 39(01): 43–53 (in Chinese)
4
Y, Chen X H, Gou W H, Liu Q M, Chen J J, Su W Lin (2017a). Advances in tree-ring stable oxygen isotope study in Asia.J Glaciol Geocryol, 39(02): 308–316 (in Chinese)
5
Z, Dong D, Mao M, Ye S, Li X, Ma S Liu (2022). Fractal features of soil grain-size distribution in a typical Tamarix cones in the Taklimakan Desert, China.Sci Rep, 12(1): 16461 https://doi.org/10.1038/s41598-022-20755-x
6
L, Ge X, Dong L, Li Q, Zhao D Yan (2018). Effects of meteorological factors on daytime transpiration of Citrus Trees.Water Saving Irrigation, 12: 17–23 (in Chinese)
7
J Gray (1981). The use of stable-isotope data in climate reconstruction. In: Wrigley T W L, Ingram M J, Farmer G, eds. Climate and History. Cambridge University Press: 53–81
8
Y, Hou N, Wang X, Zhang H, Cheng J Lu (2011). Precipitation reconstruction from tree ring width over the eastern part of the Qilian Mountains, northwestern China.Mountain Res, 29(1): 12–18 (in Chinese)
9
H Jia, J Liu, X Qin (2011). Early Holocene climatic changes and agricultural activities inferred from spore-pollen of Lop Nur. J Jilin Univ (Earth Sci Ed), 41(S1): 181–186+194 (in Chinese)
10
J Jiang (1991). Studies on resisting drought abilities of endangered species.Arid Zone Res, 8(2): 31–35 (in Chinese)
11
S Jiang, Y Yuan, W Wei, H Shang, T Zhang, R Zhang, L Qin (2016). Early summer temperature history in the Altay Mountains recorded by tree rings during 1579–2009. J Desert Res, 36(04): 1126–1132 (in Chinese)
12
L Jiao, L Ma, T Zhang, S Wang (2021). Changes of mean minimum temperature in June-July since 1798 in central Altay Mountain recorded by tree rings. Acta Ecol Sin, 41(05): 1944–1958 (in Chinese)
13
J F, Li Y J, Yuan C Y Wang (1988). Temperature sequence in the area of the middle reaches of Talimu River and ITS changes in recent 200 years.Geogr Res, 7(03): 67–71 (in Chinese)
14
M Q Li, X M Shao, W Z Nie (2022). Precipitation variation reconstructed based on tree-ring width data for the past 399 years in the eastern Yinshan Mountains, China. Chinese J App Ecol, 33(10): 2796–2804 (in Chinese)
15
Q, Li S, Zhang S, Wang Y, Fang L, Li Y Zhao (2019). The characteristics of stable oxygen isotope in Tamarix cone and climatic change in recent 400 years in Qira region, Xinjiang.Quat Sci, 39(2): 448–457 (in Chinese)
16
R, Li S, Xie Y Gu (2010). Advances in the biogeochemical study of phytolity stable isotope.Adv Earth Sci, 25(8): 812–819 (in Chinese)
17
W, Li G, Mu Y, Lin D Zhang (2021). Abrupt climatic shift at ~4000 cal. yr B.P. and late Holocene climatic instability in arid Central Asia: evidence from Lop Nur saline lake in Xinjiang, China.Sci Total Environ, 784: 147202 https://doi.org/10.1016/j.scitotenv.2021.147202
18
Z Li (2022). Research on environmental changes in Northern Lop Nur based on cations in deciduous layers of Tamarix Cones. Dissertation for Master’s Degree. Shijiazhuang Hebei Normal University (in Chinese)
19
E, Liang X, Shao N Qin (2008). Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau.Global Planet Change, 61(3–4): 313–320 https://doi.org/10.1016/j.gloplacha.2007.10.008
20
J, Liu R, Wang Y, Zhao Y Yang (2019). A 40,000-year record of aridity and dust activity at Lop Nur, Tarim Basin, northwestern China.Quat Sci Rev, 211: 208–221 https://doi.org/10.1016/j.quascirev.2019.03.023
21
Q Liu, C Gao, Y Zhao, X Xia (2013). Positive ion contained in Tamarix cone sedimentary veins and climatic and environmental change in southern region of the Taklimakan Desert. Adv Earth Sci, 28(12): 1326–1334 (in Chinese)
22
F C, Ljungqvist A, Seim P J, Krusic J F, González-Rouco J P, Werner E R, Cook E, Zorita J, Luterbacher E, Xoplaki G, Destouni E, García-Bustamante C A M, Aguilar K, Seftigen J L, Wang M H, Gagen H, Esper O, Solomina D, Fleitmann U Büntgen (2019). European warm-season temperature and hydroclimate since 850 CE.Environ Res Lett, 14(8): 084015 https://doi.org/10.1088/1748-9326/ab2c7e
23
C, Ma F, Wang Q, Cao X, Xia S, Li X Li (2008). Climate and environment reconstruction during the Medieval Warm Period in Lop Nur of Xinjiang, China.Sci Bull (Beijing), 53(19): 3016–3027 https://doi.org/10.1007/s11434-008-0366-6
24
M , Qong H , Takamura M Hudaberdi (2002). Formation and internal structure of Tamarix cones in the Taklimakan Desert.J Arid Environ, 50(1): 81–97 https://doi.org/10.1006/jare.2001.0829
25
K, Rehfeld T Laepple (2016). Warmer and wetter or warmer and dryer? Observed versus simulated covariability of Holocene temperature and rainfall in Asia.Earth Planet Sci Lett, 436: 1–9 https://doi.org/10.1016/j.epsl.2015.12.020
26
X, Shi N, Qin X, Shao Q, Wang Y Liu (2009). Precipitation change over the past 1000 years recorded in Sabina Tibetica tree rings in Lake Qinghai Basin.J Lake Sci, 21(4): 579–586 (in Chinese) https://doi.org/10.18307/2009.0418
27
Y, Shi Y, Shen R Hu (2002). Preliminary study on signal, impact and foreground of climatic shift from warm-dry to warm-humid in northwest China.J Glaciol Geocryol, 24(03): 219–226 (in Chinese)
28
Y, Shi Y, Shen D, Li G, Zhang Y, Ding R, Hu E Kang (2003). Discussion on the present climate change from Warm 2 Dry to Warm 2 Wet in northwest China.Quatern Sci, 23(2): 152–164 (in Chinese)
29
S Sun, J Huang, G Lin, W Zhao, X Han (2005). Application of stable isotope technique in the study of plant water use. Acta Ecol Sin, 25(09): 2362–2371 (in Chinese)
30
Z, Sun J, Zhang J, Zeng H, Wang Y Zhao (2013). The modern climate change revealed by the sedimentary veins of Tamarix dune in Lop Nor Region.J Arid Land Resourc Environ, 27(07): 127–133 (in Chinese)
31
J, Wang J, Li F, Chen X, Gou J, Peng P, Liu L Jin (2007). Variation of the dryness in the recent 200a derived from tree-rings width records in the east Tianshan Mountains.J Glaciol Geocryol, 29(02): 209–216 (in Chinese)
32
J Wang, Y Zhao (2011). Reconstruction of the climate parameters in Lop Nur Region over the past 160 years based on the δD and δ18O in Tamarix cone sedimentary veins. Quat Sci, 31(06): 1045–1052 (in Chinese)
33
Y, Wang Q, Feng X Kang (2016). Tree-ring-based reconstruction of temperature variability (1445–2011) for the upper reaches of the Heihe River Basin, Northwest China.J Arid Land, 8(1): 60–76 https://doi.org/10.1007/s40333-015-0138-5
34
Y Wang, G Liu, X Zhang, C Li (1982). The climatic changes recorded in the Sabina Genesis tree-rings in the Qilian Mountains, China and glacier fluctuations during the last 1000 years. Chin Sci Bull, 27(21): 1316–1319 (in Chinese)
35
Y, Wang Y Zhao (2010). Pollen assemblages of Tamarix Cone and vegetation and climatic change in the Lop Nur Region during the past about 200 years.Quat Sci, 30(03): 609–619 (in Chinese)
36
J, Wu L Ma (2011). Lake evolution and climatic and hydrological changes in arid zone of Xinjiang.Marine Geol Quat Geol, 31(2): 135–143 (in Chinese) https://doi.org/10.3724/SP.J.1140.2011.02135
37
X, Xia Y, Zhao F, Wang Q Cao (2005). Environmental significance exploration to Tamarix cone age layer in Lop Nur lake region.Chin Sci Bull, 50(20): 2395–2397 https://doi.org/10.1007/BF03183755
38
X, Xia Y, Zhao F, Wang Q, Cao G, Mu J Zhao (2004). Stratification features of Tamarix cone and its possible significance.Chin Sci Bull, 49(14): 1539–1540 https://doi.org/10.1360/03wd0104
39
L, Xie S, Huang F Li (2004). Global comparison on Palaeoclimatic change in the saline Lop Nur during the past two thousand years.Carsol Sin, 23(4): 311–316 (in Chinese)
40
L, Xie S, Huang F, Li J Zhang (2004). Global comparison on palaeoclimatic change in the Saline Luobupo during the past two thousand years.Carsol Sin,, (04): 55–60 (in Chinese)
41
G Xu, X Liu, T Chen, W An, W Wang, G Wu, X Zeng, B Wang (2015). Climatic signals of tree-ring δ18O over the western China. Quat Sci, 35(5): 1218–1226 (in Chinese)
42
J, Yao W, Mao J, Chen T Dilinuer (2021). Signal and impact of wet-to-dry shift over Xinjiang, China.Acta Geogr Sin, 76(1): 57–72
43
S, Yu Y, Yuan Q, He Z Wu (2007). Reconstruction of temperature series from A.D. 1468–2001 in the Jinghe, Xinjiang.J Glaciol Geocryol, 29: 374–379 (in Chinese)
44
R, Zhang W, Wei Y, Yuan S, Yu Q Yang (2009). A precipitation series of A.D. 1396–2005 in Aksu River Basin on the southern slopes of Tianshan Mountains: reconstruction and analysis.J Glaciol Geocryol, 31(1): 27–33 (in Chinese)
45
S, Zhang S, Wang Q, Li L, Li Y, Fang Y Zhao (2019a). The characteristics of stable oxygen isotope in Tamarix cone and climate change in recent 200 years in Andier, Xinjiang.J Arid Land Resourc Environ, 33(6): 119–125 (in Chinese)
46
T, Zhang Y, Yuan S, Yu W, Wei Q, Yang H Shang (2008). Development of two tree-ring width chronologies of the samples collected from the Baluntai region.Arid Zone Res, 25(2): 288–294 (in Chinese) https://doi.org/10.3724/SP.J.1148.2008.00288
47
X, Zhang T, Yao W, Shi Z Li (1999). Record of climate change since Little Ice Age in the ice core of the Guliya Ice Cap.J Nat Sci Hunan Normal Univ, 22(1): 81–85 (in Chinese)
Z, Zhang Y, Fang L, Li Z, Sun Y, Zhao X, Xia M Ashraf (2017). Reconstruction of the paleotemperature in the southern margin of the Taklimakan Desert based on carbon isotope discrimination of Tamarix leaves.Appl Ecol Environ Res, 15(4): 561–570 https://doi.org/10.15666/aeer/1504_561570
50
Z, Zhang I, Ullah Z, Wang P, Ma Y, Zhao X, Xia Y Li (2019b). Reconstruction of temperature for the past 400 years in the southern margin of the Taklimakan Desert based on carbon isotope fractionation of Tamarix leaves.Appl Ecol Environ Res, 17(1): 271–284 https://doi.org/10.15666/aeer/1701_271284
51
Y, Zhao G, Che H, Liu J, Zeng X Xia (2016). C and N content in organic matter of Tamarix cone and climatic and environmental change in southern region of Taklimakan desert.Arid Land Geography, 39(3): 461–467 (in Chinese)
52
Y, Zhao X, Li X, Xia X Wang (2011). C and N contents in organic matter of Tamarix dune sedimentary veins and environmental change in Lop Nur Region.J Arid Land Resourc Environ, 25(4): 149–154 (in Chinese)
53
J Zheng, X Zhang, Y Liu, Z Hao (2020). The assessment on hydroclimatic changes of different regions in China at multi-scale during the past millennium. Acta Geogr Sin, 75(7): 1432–1450 (in Chinese)
54
J, Zhou J, Wu L, Ma M Qiang (2019). Late Quaternary lake-level and climate changes in arid central Asia inferred from sediments of Ebinur Lake, Xinjiang, northwestern China.Quat Res, 92(2): 416–429 https://doi.org/10.1017/qua.2019.27
