高原湖泊中萝卜螺属壳体研究现状及展望

doi:10.18306/dlkxjz.2018.10.012

Abstract

Abstract:

Palaeohydrology and palaeohydrochemical reconstruction have always been one of the most challenging issues in lake research, and one of the main reasons for this is the lack of suitable archives. Radix sp. fossil shells are widely distributed in lakes, alluvial-lacustrine successions, and high level lake sediments on the Tibetan Plateau. These biogenic carbonate shells are a kind of promising high-resolution carrier of the environmental information. For example, the δ¹³C_shell values of the Radix shells are controlled by the δ¹³C of lake water dissolved inorganic carbon; the δ¹⁸O_shell values provide useful information about the isotopic composition of the ambient waters; and the Sr/Ca ratio of the Radix shells is significantly positively correlated with both the Sr/Ca ratio and the conductivity of the lake water. Therefore, the δ¹³C_shell and δ¹⁸O_shell values and element of the Radix sp. shells have been gradually used to provide the palaeohydrological and palaeoclimatic information on the Tibetan Plateau and other regions in existing studies. In addition, the ⁸⁷Sr/⁸⁶Sr_shell of Radix sp. reflects significantly the ⁸⁷Sr/⁸⁶Sr of the water in which the shells were formed. However, there are still many scientific issues to be explored: it is unclear how the shells of Radix sp. record the hydrological, hydrochemical, and other information of its ambient water, and how we reconstruct palaeoenvironment information based on the fossil shells of Radix sp. As a new environmental information archive, Radix sp. and their following aspects in existing research on lakes of the Tibetan Plateau were reviewed in this study, including: the classification systems of Radix sp., habitat studies of Radix sp. and applications, proxies of Radix sp. shell (δ¹³C_shell, δ¹⁸O_shell, ⁸⁷Sr/⁸⁶Sr, Sr/Ca and Mg/Ca), and palaeohydrochemical reconstruction in lakes, in order to explore the prospects for future study on Radix sp. This review found that significant unanswered questions still remain. For example, the influence of lake water chemistry and water depth on the distribution and survival of Radix sp. is unclear; it is not clear whether inter-species differences have an impact on the results of lake sediment and palaeoenvironmental studies; species level classification of Radix sp., oxygen isotope balance, and trace element need further study; and more environmental records of Radix sp. shells are needed, among others.

Key words: plateau lakes, Radix sp., stable carbon and oxygen isotopes, strontium isotope, shell element ratio, palaeohydrochemical reconstruction

Feng CHEN, Jinliang FENG. Progress and prospects of research on shells of Radix sp. in lakes on the Tibetan Plateau[J].PROGRESS IN GEOGRAPHY, 2018, 37(10): 1430-1441.

Figures/Tables 7

Fig.1

Fig.2

Fig.3

Tab.1

Published sites of lakes where living Radix sp. were found on the Tibetan Plateau"

编号	湖泊名称	文献中名称	纬度	经度	海拔/m	来源
1	太错	Tai Co	33°43′N	80°43′E	4504	Zhao et al, 2005
2	普莫雍错	Phuma Yumtso	28°29′N	90°25′E	5030	von Oheimb et al, 2011
3	班公错1	Pangong Tso	33°26′N	79°47′E	4241	von Oheimb et al, 2011
4	朗错	Lang Tso	29°12′N	87°25′E	4294	von Oheimb et al, 2011
5	冬给措纳湖1	Dongi Tsona	35°22′N	98°28′E	4090	von Oheimb et al, 2011
6	然乌湖	Rawok Tso	29°29′N	96°39′E	3913	von Oheimb et al, 2011
7	错那湖	Tso Nak	32°01′N	91°31′E	4800	von Oheimb et al, 2011
8	羊卓雍错1	Yamdrok Yumtso	29°05′N	90°22′E	4436	von Oheimb et al, 2011
9	亚当错1	Yadang Tso	29°37′N	85°44′E	5060	von Oheimb et al, 2011
10	嘎仁错	Kyering Tso	30°45′N	85°00′E	4650	von Oheimb et al, 2011
11	邦达错	Bangda Co	30°29′N	97°04′E	4450	Taft et al, 2012
12	格仁错1	Kyaring Co	31°10′N	88°10′E	4650	Taft et al, 2012
13	格仁错2	Kyaring Co	31°17′N	88°17′E	4650	Taft et al, 2012
14	冬给措纳湖2	Donggi Cona	35°15′N	98°30′E	4090	Taft et al, 2013
15	玛旁雍错	Lake Manasarovar	30°45′N	81°22′E	4595	Taft et al, 2013
16	羊卓雍错2	Yamdrok Yumco	29°02′N	90°25′E	4437	Taft et al, 2013
17	班公错2	Banggong Co	33°33′N	79°55′E	4250	Taft et al, 2013
18	达热不错	Tarab Co	32°26′N	83°12′E	4450	Taft et al, 2013
19	亚当错2	Yadang Co	29°39′N	85°44′E	5060	Taft et al, 2013
20	昂拉仁错	Ngangla Ring Tso	31°27′N	83°21′E	4689	Hudson et al, 2015
21	纳木错1	Nam Co	30°47′N	90°16′E	4728	Chen et al, 2016
22	纳木错2	Nam Co	30°53′N	90°14′E	4728	Chen et al, 2016
23	纳木错3	Nam Co	30°55′N	90°57′E	4728	Chen et al, 2016
24	纳木错4	Nam Co	30°53′N	90°52′E	4728	Chen et al, 2016
25	白马纳木错	Baima Nam Co	30°46′N	90°57′E	4438	Chen et al, 2016
26	空姆错	Gongmo Tso	28°59′N	90°23′E	4438	Chen et al, 2016
27	沉错	Chen Co	28°57′N	90°29′E	4434	Chen et al, 2016
28	巴纠错	Pagyu¨ Tso	28°44′N	90°50′E	4511	Chen et al, 2016
29	羊卓雍错3	Yamdrok Yumtso	28°46′N	90°31′E	4436	Chen et al, 2016
30	羊卓雍错4	Yamdrok Yumtso	28°50′N	91°03′E	4444	Chen et al, 2016
31	农针错	Nongzhen Tso	28°53′N	90°24′E	4564	Chen et al, 2016
32	姆错丙尼	Mucuobingni	30°33′N	86°17′E	4680	Chen et al, 2016
33	恰规错	Qiagui Co	31°51′N	88°17′E	4552	Chen et al, 2016
34	色林错	Selin Co	31°47′N	88°26′E	4545	Chen et al, 2016
35	纳木错5	Nam Co	30°55′N	90°53′E	4728	Chen et al, 2017

Tab.1

Fig.4

Tab.2

Fig.5

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编号	现代壳体⁸⁷Sr/⁸⁶Sr	性质	湖水⁸⁷Sr/⁸⁶Sr	性质	相对变化
21	0.713655	纳木错现代壳体	0.713753	相应点湖水	0.000098
24	0.713860	纳木错现代壳体	0.713694	相应点湖水	0.000165
29	0.709575	羊卓雍错现代壳体	0.709760	相应点湖水	0.000185

Progress and prospects of research on shells of Radix sp. in lakes on the Tibetan Plateau

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