Testing the standardized growth curve (SGC) to OSL dating coastal sediments from the South Bohai Sea, China

• Autorzy: Guang-Quan Ch. , Liang Y. , Xing-Yong X , Hong-Jun Y. , Jian-Rong C. , Qiao S. , Lin-Hai Y. , Yong-Hang X. , Jun-Yi G. , Zhong-Ping L.
• Języki publikacji: EN

Abstrakty

EN

It has been suggested that the standardized growth curve (SGC) method can be used to ac-curately determinate equivalent dose (De) and reduce measurement time. However, different opinions regarding the applicability of the SGC method exist. In this paper, we evaluated quartz OSL SGCs of marine and coastal sediments of different grain sizes and different cores in the south Bohai Sea in China, and tested their applicability to the determination of De values. Our results suggested as fol-lows: (1) The SGC method is applicable to both multiple- and single- aliquot regenerative-dose (MAR and SAR) protocols of OSL dating and efficiently provides reliable estimates of De. (2) Fine-sand quartz of different palaeodoses showed highly similar dose-response curves and an SGC was de-veloped, but old samples using the SGC method have large uncertainties. (3) For coarse-silt quartz, two different types of dose-response curves were recorded: low-dose (≤60Gy) and high-dose (≥100Gy). The growth curves of low-dose quartz were similar to each other, facilitating the use of SGC in De estimations, but errors tended to be larger than those obtained in the SAR method. For high-dose (100-300Gy) quartz, the SGC was also found to be reliable, but there was large uncertainty in De (>300Gy) estimation. We suggest that SGC could be employed for the dating of marine and coastal sediments dating using either MAR or SAR OSL protocol and either fine-silt, coarse-silt or fi-ne-sand quartz.

Słowa kluczowe

EN

Standardized growth curve (SGC); OSL dating; marine sediments; Bohai Sea in China

• Wydawca: De Gruyter
• Czasopismo: Geochronometria
• Rocznik: 2013
• Tom: Vol. 40, no. 2
• Strony: 101--112
• Opis fizyczny: Bibliogr. 39 poz., rys., wykr.

Twórcy

autor

Guang-Quan Ch.

• State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China
• Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China

autor

Liang Y.

• State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

autor

Xing-Yong X

• Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China

autor

Hong-Jun Y.

• Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China

autor

Jian-Rong C.

• Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China
• College of Environment and Planning, Liaocheng University, Liaocheng 252059, China

autor

Qiao S.

• Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China

autor

Lin-Hai Y.

• State Key Laboratory of Cryosphere Sciences, Cold and Arid Regions Environment and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China

autor

Yong-Hang X.

• Open Laboratory of Ocean & Coast Environmental Geology, Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China

autor

Jun-Yi G.

• The Laboratory of Human Evolution, Institute of Vertebrate Palaeontology and Palaeoanthropology, Chinese Academy of Sciences, Beijing 100044, China

autor

Zhong-Ping L.

• State Key Laboratory of Cryosphere Sciences, Cold and Arid Regions Environment and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China

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