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Journal articles on the topic 'TT-OSL'

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Author: Grafiati

Published: 10 December 2022

Last updated: 28 January 2023

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1

Faershtein, Galina, Naomi Porat, and Ari Matmon. "Extended-range luminescence dating of quartz and alkali feldspar from aeolian sediments in the eastern Mediterranean." Geochronology 2, no. 1 (May 7, 2020): 101–18. http://dx.doi.org/10.5194/gchron-2-101-2020.

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Abstract. Optically stimulated luminescence (OSL) of quartz is an established technique for dating late Pleistocene to late Holocene sediments. Unfortunately, this method is often limited to up to 100 ka (thousands of years). Recent developments in new extended-range luminescence techniques show great potential for dating older sediments of middle and even early Pleistocene age. These methods include thermally transferred OSL (TT-OSL) and violet stimulated luminescence (VSL) for quartz and post-infrared infrared stimulated luminescence (pIRIR) for feldspar. Here we investigate the luminescence behaviour of the TT-OSL, VSL, and pIRIR signals of quartz and feldspar minerals of aeolian sediments of Nilotic origin from the eastern Mediterranean. We sampled a 15 m thick sequence (Kerem Shalom) comprising sandy calcic palaeosols, which is part of a sand sheet that covers an extensive region in south-western Israel. Dose recovery and bleaching experiments under natural conditions indicated that the pIRIR250 signal is the most suitable for dating the Nilotic feldspar. Luminescence intensity profiles revealed natural saturation of the three signals at the same depth of ∼6 m, indicating that ages of samples below that depth are minimum ages. Using TT-OSL and pIRIR250, a minimum age of 715 ka for the base of the section was obtained, suggesting aeolian sand accumulation along the eastern Mediterranean coastal plain already since the early Pleistocene. Our results indicate that both TT-OSL and pIRIR250 can accurately date aeolian sediments of Nilotic origin up to 200 ka and that minimum ages can be provided for older samples up to the early Pleistocene.

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2

Porat, N., G. A. T. Duller, H. M. Roberts, and A. G. Wintle. "A simplified SAR protocol for TT-OSL." Radiation Measurements 44, no. 5-6 (May 2009): 538–42. http://dx.doi.org/10.1016/j.radmeas.2008.12.004.

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3

Chapot, M. S., H. M. Roberts, G. A. T. Duller, and Z. P. Lai. "Natural and laboratory TT-OSL dose response curves: Testing the lifetime of the TT-OSL signal in nature." Radiation Measurements 85 (February 2016): 41–50. http://dx.doi.org/10.1016/j.radmeas.2015.11.008.

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4

Hernandez, Marion, Barbara Mauz, Norbert Mercier, and Zhixiong Shen. "Evaluating the efficiency of TT-OSL SAR protocols." Radiation Measurements 47, no. 9 (September 2012): 669–73. http://dx.doi.org/10.1016/j.radmeas.2012.04.017.

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5

Arnold, Lee J., Martina Demuro, Nigel A. Spooner, Gavin J. Prideaux, Matthew C. McDowell, Aaron B. Camens, Elizabeth H. Reed, et al. "Single-grain TT-OSL bleaching characteristics: Insights from modern analogues and OSL dating comparisons." Quaternary Geochronology 49 (February 2019): 45–51. http://dx.doi.org/10.1016/j.quageo.2018.01.004.

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6

Faershtein, G., N. Porat, and A. Matmon. "Natural saturation of OSL and TT-OSL signals of quartz grains from Nilotic origin." Quaternary Geochronology 49 (February 2019): 146–52. http://dx.doi.org/10.1016/j.quageo.2018.04.002.

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7

Faershtein, Galina, Benny Guralnik, Renske Lambert, Ari Matmon, and Naomi Porat. "Investigating the thermal stability of TT-OSL main source trap." Radiation Measurements 119 (December 2018): 102–11. http://dx.doi.org/10.1016/j.radmeas.2018.09.010.

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8

Adamiec, G., G. A. T. Duller, H. M. Roberts, and A. G. Wintle. "Improving the TT-OSL SAR protocol through source trap characterisation." Radiation Measurements 45, no. 7 (August 2010): 768–77. http://dx.doi.org/10.1016/j.radmeas.2010.03.009.

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9

Pagonis, V., A. G. Wintle, R. Chen, and X. L. Wang. "A theoretical model for a new dating protocol for quartz based on thermally transferred OSL (TT-OSL)." Radiation Measurements 43, no. 2-6 (February 2008): 704–8. http://dx.doi.org/10.1016/j.radmeas.2008.01.025.

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10

Zander, A., and A. Hilgers. "Testing the potential of OSL, TT-OSL, IRSL and post-IR IRSL luminescence dating on a Middle Pleistocene sediment record of Lake El'gygytgyn, Russia." Climate of the Past Discussions 8, no. 5 (September 28, 2012): 4779–815. http://dx.doi.org/10.5194/cpd-8-4779-2012.

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Abstract. Lake El'gygytgyn is a 12 km wide crater lake located in remote Chukotka in the far East Russian Arctic about 100 km to the north of the Arctic Circle. It was formed by a meteorite impact about 3.58 Ma ago. This study tests the paleomagnetic and proxy data-based Mid- to Late-Pleistocene sediment deposition history using novel luminescence dating techniques of sediment cores taken from the centre of the 175 m deep lake. For dating polymineral and quartz fine grains (4–11 μm grain size range) were extracted from nine different levels from the upper 28 m of sediment cores 5011-1A and 5011-1B. Polymineral sub-samples were analysed by infra-red stimulated luminescence (IRSL) and post-IR infra-red stimulated luminescence (post-IR IRSL) using single aliquot regenerative dose (SAR) sequences. SAR protocols were further applied to measure the blue light optically stimulated luminescence (OSL) and thermally-transferred OSL (TT-OSL) of fine-grained quartz supplemented by a multiple aliquot TT-OSL approach. According to an independent age model, the lowest sample from 27.8–27.9 m below lake bottom level correlates to the Brunhes-Matuyama (B/M) reversal. Finally, the SAR post-IR-IRSL protocol applied to polymineral fine grains was the only luminescence technique able to provide dating results of acceptable accuracy up to ca. 700 ka. Major factors limiting precision and accuracy of the luminescence chronology are, for some samples, natural signals already approaching saturation level, and overall the uncertainty related to the sediment water content and its variations over geological times.

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11

Biswas, R. H. "Development and Application of Luminescence to Earth and Planetary Sciences: Some Landmarks." Defect and Diffusion Forum 357 (July 2014): 217–43. http://dx.doi.org/10.4028/www.scientific.net/ddf.357.217.

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Luminescence, mainly thermoluminescence (TL) and optically stimulated luminescence (OSL), has been researched for more than five decades towards its application to earth and planetary sciences. Luminescence production mechanism has been understood through several theoretical studies, like analytical kinetic theory, numerical models along with the experimental results. Instrument development has progressed with aim from user friendly TL/OSL reader dedicated for dating to challenging reader forin-situMartian sediment dating. Since the development of optical dating in 1985, the technique revolutionised the research in earth sciences. And since then to recent, many methodologies have been developed and some are in developing stage using different signals, like, single grain OSL, red TL, time resolved OSL, thermally transferred OSL (TT-OSL), post infrared-infrared stimulated luminescence (pIR-IRSL), violet light stimulated luminescence (VSL), infrared radioluminescence (IRRL), etc. with an objective to improve the accuracy and precision and to extend the dating range. The wide range of application in different environment, e.g. aeolian, fluvial, marine, glacier, soil, volcanic materials, heated materials, shocked materials, meteorites, etc. have made the technique successful to understand the quaternary history of earth and planetary information like terrestrial and cosmic ray exposure ages of meteorite, meteoroid orbit, thermal metamorphism history of meteorite etc. The aim of this present paper is to discuss some landmarks and recent trends in the development and application in these areas. Contents of the Paper

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12

Yukihara, E. G. "Observation of strong thermally transferred optically stimulated luminescence (TT-OSL) in BeO." Radiation Measurements 121 (February 2019): 103–8. http://dx.doi.org/10.1016/j.radmeas.2018.12.014.

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13

Yukihara, E. G. "Characterization of the thermally transferred optically stimulated luminescence (TT-OSL) of BeO." Radiation Measurements 126 (July 2019): 106132. http://dx.doi.org/10.1016/j.radmeas.2019.106132.

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14

Kim, J. C., G. A. T. Duller, H. M. Roberts, A. G. Wintle, Y. I. Lee, and S. B. Yi. "Re-evaluation of the chronology of the palaeolithic site at Jeongokri, Korea, using OSL and TT-OSL signals from quartz." Quaternary Geochronology 5, no. 2-3 (April 2010): 365–70. http://dx.doi.org/10.1016/j.quageo.2009.02.005.

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15

Stevens, T., J. P. Buylaert, and A. S. Murray. "Towards development of a broadly-applicable SAR TT-OSL dating protocol for quartz." Radiation Measurements 44, no. 5-6 (May 2009): 639–45. http://dx.doi.org/10.1016/j.radmeas.2009.02.015.

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16

Liu, Jinfeng, Andrew S. Murray, Mayank Jain, Jan-Pieter Buylaert, Yanchou Lu, and Jie Chen. "Developing a SAR TT-OSL protocol for volcanically-heated aeolian quartz from Datong (China)." Quaternary Geochronology 10 (July 2012): 308–13. http://dx.doi.org/10.1016/j.quageo.2012.02.008.

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17

Yi, Shuangwen, Huayu Lu, and Thomas Stevens. "SAR TT-OSL dating of the loess deposits in the Horqin dunefield (northeastern China)." Quaternary Geochronology 10 (July 2012): 56–61. http://dx.doi.org/10.1016/j.quageo.2012.03.011.

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18

Zander, A., and A. Hilgers. "Potential and limits of OSL, TT-OSL, IRSL and pIRIR<sub>290</sub> dating methods applied on a Middle Pleistocene sediment record of Lake El'gygytgyn, Russia." Climate of the Past 9, no. 2 (March 14, 2013): 719–33. http://dx.doi.org/10.5194/cp-9-719-2013.

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Abstract. This study tests the paleomagnetic and proxy-data based Mid- to Upper Pleistocene sediment deposition history of Lake El'gygytgyn by applying different approaches of luminescence dating techniques on sediment cores taken from the centre of the 175 m deep lake. For dating polymineral and quartz fine grains (4–11 μm grain size range) were extracted from nine different levels from the upper 28 m of sediment cores 5011-1A and 5011-1B. According to the independent age model, the lowest sample from 27.8–27.9 m below lake bottom level correlates to the Brunhes-Matuyama (B/M) reversal. Polymineral sub-samples were analysed by infra-red stimulated luminescence (IRSL) and post-IR IRSL measured at 290 °C (pIRIR290) using single aliquot regenerative dose (SAR) sequences. SAR protocols were further applied to measure the blue light optically stimulated luminescence (OSL) and thermally-transferred OSL (TT-OSL) of fine-grained quartz supplemented by a multiple aliquot approach. Neither low temperature IRSL measurements at 50 °C nor any OSL dating approach on quartz yielded reliable results. Deconvolution of their dose response curves revealed a pseudo-increase of the dose response curves and explains the observed underestimation. The pIRIR protocol applied to polymineral fine grains was the only luminescence technique able to provide dating results of acceptable accuracy up to ca. 700 ka when correlated to the existing proxy-data and paleomagnetic based age record. We present the potential and limits of the different dating techniques and a correlation of pIRIR290 results with the proxy-data based age model.

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19

Sun, Xuefeng, Shuangwen Yi, Huayu Lu, and Wenchao Zhang. "TT-OSL and post-IR IRSL dating of the Dali Man site in central China." Quaternary International 434 (April 2017): 99–106. http://dx.doi.org/10.1016/j.quaint.2015.05.027.

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20

Arnold, Lee J., and Martina Demuro. "Insights into TT-OSL signal stability from single-grain analyses of known-age deposits at Atapuerca, Spain." Quaternary Geochronology 30 (October 2015): 472–78. http://dx.doi.org/10.1016/j.quageo.2015.02.005.

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21

Tsukamoto, Sumiko, Geoff A. T. Duller, and Ann G. Wintle. "Characteristics of thermally transferred optically stimulated luminescence (TT-OSL) in quartz and its potential for dating sediments." Radiation Measurements 43, no. 7 (August 2008): 1204–18. http://dx.doi.org/10.1016/j.radmeas.2008.02.018.

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22

Hernandez, Marion, Norbert Mercier, Jean-Philippe Rigaud, Jean-Pierre Texier, and Françoise Delpech. "A revised chronology for the Grotte Vaufrey (Dordogne, France) based on TT-OSL dating of sedimentary quartz." Journal of Human Evolution 75 (October 2014): 53–63. http://dx.doi.org/10.1016/j.jhevol.2014.05.010.

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23

Hernandez, Marion, Norbert Mercier, Pascal Bertran, David Colonge, and Laure Amélie Lelouvier. "Premiers éléments de datation des industries du Pléistocène moyen (Acheuléen - Paléolithique moyen ancien) de la région pyrénéo-garonnaise : une approche géochronologique pluri-méthodes (TL, OSL et TT-OSL)." Paléo, no. 23 (December 15, 2012): 155–70. http://dx.doi.org/10.4000/paleo.2344.

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24

Bartz, M., L. J. Arnold, M. Demuro, M. Duval, G. E. King, G. Rixhon, C. Álvarez Posada, J. M. Parés, and H. Brückner. "Single-grain TT-OSL dating results confirm an Early Pleistocene age for the lower Moulouya River deposits (NE Morocco)." Quaternary Geochronology 49 (February 2019): 138–45. http://dx.doi.org/10.1016/j.quageo.2018.04.007.

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25

Rosenberg, T. M., F. Preusser, and A. G. Wintle. "A comparison of single and multiple aliquot TT-OSL data sets for sand-sized quartz from the Arabian Peninsula." Radiation Measurements 46, no. 6-7 (June 2011): 573–79. http://dx.doi.org/10.1016/j.radmeas.2011.03.020.

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26

Sun, Xuefeng, Huayu Lu, Shejiang Wang, Shuangwen Yi, Chen Shen, and Wenchao Zhang. "TT-OSL dating of Longyadong Middle Paleolithic site and paleoenvironmental implications for hominin occupation in Luonan Basin (central China)." Quaternary Research 79, no. 2 (March 2013): 168–74. http://dx.doi.org/10.1016/j.yqres.2012.10.003.

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AbstractDating middle Pleistocene hominin occupations alongside the reconstruction of paleoenvironments in China between 700 and 100 ka has always been a challenging task. In this paper, we report thermally transferred optically stimulated luminescence (TT-OSL) dating results for a Middle Paleolithic site in the Luonan Basin, central China, which we have named Longyadong Cave. The results suggest that the age of cave infilling and the deposition of sediments outside the cave range between 389 ± 18 and 274 ± 14 ka. These deposits are stratigraphically and geochronologically correlated with the L4 loess and S3 paleosol units of the typical loess–paleosol sequence of the Chinese Loess Plateau, and with Marine Isotope Stages (MIS) 10 to 9, respectively. On the basis of these new ages and the available paleoenvironmental data, it is suggested that the Longyadong hominins might have occupied the site both in glacial and interglacial periods, demonstrating that they coped well with environmental change in this mountainous region in warm/wet and cold/dry climates. The study further implies that the hominins abandoned the Longyadong Cave between 274 ± 14 and 205 ± 19 ka, when it was sealed by alluvial and slope deposits.

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27

Neudorf, Christina M., Olav B. Lian, Peter D. McIntosh, Travis B. Gingerich, and Paul C. Augustinus. "Investigation into the OSL and TT-OSL signal characteristics of ancient (>100 ka) Tasmanian aeolian quartz and its utility as a geochronometer for understanding long-term climate-driven landscape change." Quaternary Geochronology 53 (August 2019): 101005. http://dx.doi.org/10.1016/j.quageo.2019.101005.

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28

Thiel, Christine, Jan-Pieter Buylaert, Andrew S. Murray, Noureddine Elmejdoub, and Younes Jedoui. "A comparison of TT-OSL and post-IR IRSL dating of coastal deposits on Cap Bon peninsula, north-eastern Tunisia." Quaternary Geochronology 10 (July 2012): 209–17. http://dx.doi.org/10.1016/j.quageo.2012.03.010.

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29

Hernandez, Marion, Norbert Mercier, Pascal Bertran, David Colonge, and Laure Amélie Lelouvier. "First dating results for the Middle Pleistocene industries (Acheulean – Early Middle Palaeolithic) in the Pyrenees – Garonne region: a multi methods geochronological approach (TL, OSL and TT-OSL) of the Duclos and Roment." Paléo, no. 23 (December 15, 2012): 155–70. http://dx.doi.org/10.4000/paleo.2466.

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30

Pickering, Robyn, Zenobia Jacobs, Andy I. R. Herries, Panagiotis Karkanas, Miryam Bar-Matthews, Jon D. Woodhead, Peter Kappen, Erich Fisher, and Curtis W. Marean. "Paleoanthropologically significant South African sea caves dated to 1.1–1.0 million years using a combination of U–Pb, TT-OSL and palaeomagnetism." Quaternary Science Reviews 65 (April 2013): 39–52. http://dx.doi.org/10.1016/j.quascirev.2012.12.016.

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31

Brown, Nathan D., and Steven L. Forman. "Evaluating a SAR TT-OSL protocol for dating fine-grained quartz within Late Pleistocene loess deposits in the Missouri and Mississippi river valleys, United States." Quaternary Geochronology 12 (October 2012): 87–97. http://dx.doi.org/10.1016/j.quageo.2012.06.008.

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32

Liu, Jinfeng, Andrew S. Murray, Jan-Pieter Buylaert, Mayank Jain, Jie Chen, and Yanchou Lu. "Stability of fine-grained TT-OSL and post-IR IRSL signals from ac. 1 Ma sequence of aeolian and lacustrine deposits from the Nihewan Basin (northern China)." Boreas 45, no. 4 (May 18, 2016): 703–14. http://dx.doi.org/10.1111/bor.12180.

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33

Hernandez, Marion, Jean-Jacques Bahain, Norbert Mercier, Olivier Tombret, Christophe Falguères, and Jacques Jaubert. "Dating results on sedimentary quartz, bones and teeth from the Middle Pleistocene archaeological site of Coudoulous I (Lot, SW France): A comparative study between TT-OSL and ESR/U-series methods." Quaternary Geochronology 30 (October 2015): 493–97. http://dx.doi.org/10.1016/j.quageo.2015.06.003.

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34

Rodrigues, Fernanda Costa G., Naomi Porat, Thays Desiree Mineli, Ian Del Río, Pontien Niyonzima, Luciana Nogueira, Fabiano do Nascimento Pupim, et al. "Extended-Range Luminescence Dating of Central and Eastern Amazonia Sandy Terrains." Frontiers in Earth Science 10 (July 6, 2022). http://dx.doi.org/10.3389/feart.2022.888443.

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The Amazonia biome hosts upland closed and open vegetation ecosystems, in which the current biogeographical patterns relate to the evolution of the physical landscape. Therefore, understanding the origin and timing of the substrates supporting different ecosystems is indispensable for better comprehension of Amazonian biogeography. Here we used quartz optically stimulated luminescence (OSL) and thermally transferred optically stimulated luminescence (TT-OSL) for dating sandy substrates of closed and open vegetation environments in Central and Eastern Amazonia, from both outcrop and drill core samples (Autazes core: PBAT-15-43). These sandy substrates present ages ranging from 1 ka up to almost 2 Ma, that were primarily interpreted as depositional ages of fluvial terraces. Moreover, ages are discussed in terms of potential geomorphic processes leading to the formation of substrates, such as soil mixing and apparent age of quartz from the parent bedrock. The coupling between OSL and TT-OSL techniques allow us to date sedimentary deposits covering the whole Quaternary, which implies a new time window for the Amazonia history.

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35

Lai, Hai-Cheng, Yi-Yuan Li, Jia-Fu Zhang, and Liping Zhou. "Chronology of the Huxushan Paleolithic site in south China: Inferred from multiple luminescence dating techniques." Geochronometria, March 25, 2021. http://dx.doi.org/10.2478/geochr-2020-0039.

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Abstract The Huxushan archaeological site in northern Hunan Province, China, was recently excavated, from which stone tools including handaxes were unearthed. The deposits of the site are chemically weathered, which makes it difficult to date the site using numerical dating techniques except for optically stimulated luminescence (OSL) method. Here, we used various luminescence procedures including single-aliquot regenerative-dose (SAR), sensitivity-corrected multiple-aliquot regenerative-dose (SMAR) and thermally transferred optically stimulated luminescence (TT-OSL) SAR procedures on fine-grained quartz, and two-step post-infrared infrared stimulated luminescence (pIRIR) and multi-elevated-temperature pIRIR (MET-pIRIR) procedures on fine polymineral fractions. The results show that the fine quartz grains have excellent luminescence properties and the quartz SAR-, SMAR- and TT-OSL ages for the samples agree with each other and in stratigraphical order except for one sample. The fine polymineral fractions exhibited relatively weak pIRIR and MET-pIRIR signals, resulting in difficulty in constructing the dose-response curve for MET-pIRIR signals and the stratigraphically inconsistent pIRIR(100, 275) ages. The seven samples yielded their quartz OSL ages ranging from about 62 ka to 133 ka. The two samples from the cultural layer was dated to 78 to 92 ka using different procedures on fine quartz . However, given the systematically older pIRIR ages obtained with the fine polymineral grains for the two samples, their quartz OSL ages are considered to represent the minimal ages of this layer, and their pIRIR(100, 275) ages of 118 and 110 ka represent the upper age limit, indicating that the site was occupied by hominins during Marine Isotope Stage 5.

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36

Richard, Maïlys, Michael Chazan, and Naomi Porat. "Single grain TT-OSL ages for the Earlier Stone Age site of Bestwood 1 (Northern Cape Province, South Africa)." Quaternary International, August 2020. http://dx.doi.org/10.1016/j.quaint.2020.08.019.

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37

Jacobs, Zenobia, Richard G. Roberts, Terry J. Lachlan, Panagiotis Karkanas, Curtis W. Marean, and David L. Roberts. "Development of the SAR TT-OSL procedure for dating Middle Pleistocene dune and shallow marine deposits along the southern Cape coast of South Africa." Quaternary Geochronology, April 2011. http://dx.doi.org/10.1016/j.quageo.2011.04.003.

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