|Table of Contents|

Review on Formation of Lacustrine Carbonate Minerals and Their Paleoclimate Significance(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2022年第02期
Page:
156-170
Research Field:
环境与可持续发展
Publishing date:

Info

Title:
Review on Formation of Lacustrine Carbonate Minerals and Their Paleoclimate Significance
Author(s):
LAN Min-wen123 SONG You-gui12* CHENG Liang-qing123
(1. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, Shaanxi, China; 2. CAS Center for Excellence in Quaternary Science and Global Change, Xi'an 710061, Shaanxi, China; 3. University of Chinese Academy of Sciences, Beijing 100049, China)
Keywords:
mineralogy global change paleoclimate paleoenvironment lacustrine sediment carbonate carbon isotope oxygen isotope
PACS:
P57; P92
DOI:
10.19814/j.jese.2021.08035
Abstract:
Carbonate minerals in the lacustrine sediments bear abundant geological and environmental information, such as regional geological background, sedimentary process, the changes of climatic and environmental conditions, the activities of aquatic organisms and physical-chemical properties of lake water. Thus, they have become one of the important approaches for paleoclimatic reconstruction. Based on the previous literatures, the factors controlling the formation of lacustrine carbonates and the changes of carbon and oxygen isotopic compositions were summarized, the paleoclimatic significance was interpreted, the application progress of lacustrine carbonates in paleoclimate and paleoenvironment reconstructions was reviewed, and some problems existing in the application of lacustrine carbonate were also pointed out. Furthermore, the development trend in this field for future research was proposed. The results show that the formation of lacustrine carbonates is related to temperature, precipitation, biological activity, lake hydrology and physical-chemical properties of lake water; therefore, the fluctuation of carbonate content can indicate the temperature, effective humidity, water inflow, biological activity and even the intensity of the dominant wind in this region; stable oxygen(δ18O)and carbon(δ13C)isotope compositions of carbonates are common proxies in paleolimnological studies, which can be used for reconstructing various climatic and environmental parameters including temperature, effective humidity, productivity, physical-chemical properties of lake water, the change of water vapor source and transmission path related to the atmospheric circulation and paleoflood events. The paleoclimatic significance of lacustrine carbonate is becoming richer and more complex, and it will continue to play a pivotal role in the future paleoclimate research.

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