School of Geography and the Environment, University of Oxford

Luminescence dating is used to identify when a sample was last exposed to daylight or extreme heat by estimating the amount of ionising radiation absorbed since burial or firing. This equation very simply expresses the calculations necessary, but it is important to be aware of the factors influencing the two values used. Heterogeneous sediments and radioactive disequilibria will increase errors on Dr, while incomplete bleaching of the sample prior to burial, anomalous fading in feldspars, and the estimation of past sediment moisture content may all also add to increased errors. The dating of sediments using the luminescence signal generated by optical stimulation OSL offers an independent dating tool, and is used most often on the commonly occurring minerals of quartz and feldspar and, as such, has proved particularly useful in situations devoid of the organic component used in radiocarbon dating. Quartz has been used for dating to at least ka, while the deeper traps of feldspar have produced dates as old as 1 ma. The use of fine-grain dating for samples such as pottery, loess, burnt flint and lacustrine sediments, and coarse-grain dating of aeolian, fluvial and glacial sediments is regularly undertaken. While thermoluminescence TL, the generation of a luminescence signal generated by thermal stimulation is still conducted on pottery and burnt flint samples, the bulk of luminescence dating now uses optical stimulation as this releases a signal that is far more readily zeroed than that re-set by heat. Analysis of fully bleached samples is preferred as this ensures that associated errors are kept to a minimum.

Dr Jean-Luc Schwenninger

Susan Squibb a. Sue Bird is a part-time D. Her research focuses on 2 archives from the Geography collections, now in the Radcliffe Science Library but originating in the departmental library of the School. One is the teaching glass slide collection, augmented by personal slides, both glass and 35mm, taken by a number of former academics; the other a remarkable survival of undergraduate dissertations beginning in which includes their photographs taken in the field.

Radiocarbon Laboratory. University of Waikato Radiocarbon Dating Laboratory​. Oxford University – Research Lab for Archaeology and Radiocarbon Accelerator Unit. SURRC Radiocarbon Luminescence Dating Laboratory Aberystwyth.

The impetus behind this study is to understand the sedimentological dynamics of very young fluvial systems in the Amazon River catchment and relate these to land use change and modern analogue studies of tidal rhythmites in the geologic record. Many of these features have an appearance of freshly deposited pristine sand, and these observations and information from anecdotal evidence and LandSat imagery suggest an apparent decadal stability.

Signals from medium-sized aliquots 5 mm diameter exhibit very high specific luminescence sensitivity, have excellent dose recovery and recycling, essentially independent of preheat, and show minimal heat transfer even at the highest preheats. Significant recuperation is observed for samples from two of the study sites and, in these instances, either the acceptance threshold was increased or growth curves were forced through the origin; recuperation is considered most likely to be a measurement artefact given the very small size of natural signals.

Despite the use of medium-sized aliquots to ensure the recovery of very dim natural OSL signals, these results demonstrate the potential of OSL for studying very young active fluvial processes in these settings. An important facet of the development of a geochronological technique is the investigation of potential age range.

Much recent work in the luminescence field has focused on maximum achievable ages using high-temperature post-infrared infrared pIRIR signals from feldspars [ 1 , 2 ]. In contrast for quartz optically stimulated luminescence OSL , the more efficient signal resetting coupled with environments where grain reworking is evident make it well suited to assessment of minimum achievable age. Notable examples are studies of young fluvial deposits [ 3 , 4 , 5 , 6 ] and dunes [ 7 , 8 , 9 , 10 , 11 ].

Regarding the application of OSL dating to fluvial sediments in the Amazon region, a number of studies have used the technique to try to constrain the origin and development of the drainage system, documenting Mid—Late Pleistocene ages [ 12 , 13 , 14 ], and OSL analyses have also been carried out to investigate the Late Pleistocene to Holocene development of fluvial bars [ 15 ].

The impetus behind this work was to investigate the feasibility of optically stimulated luminescence OSL dating of very young fluvial and shoreline landforms in the Amazon River catchment. The ultimate goal of the study is to use OSL to help understand the sedimentological dynamics of fluvial systems in the Amazon.


Scientists in North America first developed thermoluminescence dating of rock minerals in the s and s, and the University of Oxford, England first developed the thermoluminescence dating of fired ceramics in the s and s. During the s and s scientists at Simon Frasier University, Canada, developed standard thermoluminescence dating procedures used to date sediments.

In , they also developed optically stimulated luminescence dating techniques, which use laser light, to date sediments. The microscopic structure of some minerals and ceramics trap nuclear radioactive energy.

Postdoctoral Research Fellow, University of Oxford, U.K., I am currently setting-up a new luminescence dating laboratory with state-of-the art.

This site is using cookies to collect anonymous visitor statistics and enhance the user experience. Science Classification details. Abstract: Without robust age control, reconstructing the past dynamics of the Earth system in response to external forcing is problematic. Chronometry is a critical part of studying past environmenst, climates, ecology, human evolution and human landscape-use. Several excellent methods for dating ancient material exist.

In many environmental contexts, however, optically-stimulated luminescence OSL dating is the only method than can be used, due to the nature of the sediments that preserve the environmental record. The Oxford laboratory has long-running research excellence in studying the last approximately , years of Earth’s terrestrial history, specifically in African and other dryland regions, including Arabia, India and China. These studies have focused on changes in landscape conditions, including ancient lakes and rivers, and on questions of archaeology and human evolution, including responses to environmental change and mobility.

The extent and conviction with which such studies can make conclusions is affected strongly by the quality and range of the chronology available. Having greater confidence in the dates derived from analysed sediments, and being able to extend the age range beyond what is currently possible, would allow a host of new research questions to be addressed that would greatly advance these fields. This includes establishing long up to 1Ma terrestrial records of climate change, much needed by both the archaeological and modelling communities, making major contributions to our understanding of both human prehistory, past climate changes and, ultimately improvements to model predictions of future climate change.

Primary Menu

Chronometric Dating in Archaeology pp Cite as. The basic principles are explained in terms of thermoluminescence dating of pottery, with particular regard for the interests of archaeologists. Extensions of luminescence dating to other fired materials such as burnt flint, and to stalagmitic calcite and unburnt sediment are then outlined, including optical dating of the latter.

Final sections deal with limitations in age range, accuracy and error limits. Unable to display preview.

of the quality of performance of the new luminescence dating laboratory at the Instituto Tecnológico e calibrated versus the Oxford and the Gif-sur-Yvette.

We use cookies on our website. To learn more about the cookies we use, please see our cookie policy. You can manage cookies via your browser settings. By continuing to browse the site you are agreeing to our use of cookies. Accept and Close. Please note: This is version 1.

Testing Luminescence Dating Methods for Small Samples from Very Young Fluvial Deposits

Email: aayush. For his doctoral research, Aayush is doing a detailed palaeoenvironmental analysis of the Thar Desert in India by establishing a geochronology of aeolian accumulations during the late Quaternary period. It will include use of OSL dating applications and modelling to establish and further develop the dune accumulation records as proxies of desert climate change. The Thar Desert, NW India, the most densely populated desert in the world, lies at the limit of the region receiving precipitation from the Indian summer monsoon, with a modern mean NE-W rainfall gradient of mm to less than m.

In addition to dating per se, the Luminescence Dating Laboratory has interests in the for sediment dosimetry based on measurements in the “Oxford blocks”.

Instrumental data have recorded rapid warming during recent decades in this region, approximately three times faster than that of the global average Zhang et al. Long-term records derived from paleoclimatic proxies are invaluable for improving our understanding of the natural range and causes of variability in regions compared with instrumental records. There are over lakes larger than 1 km 2 distributed across the TP Wang and Dou, ; Ma et al.

The storage of water in a closed lake basin reflects the balance between evaporation and water influx, referring to both runoff and direct precipitation Benson and Paillet, , and it has typically been used to infer the variation history in the regional effective moisture e. Outcrops and landforms can provide direct evidence of sediment facies changes, and record details of lake-level fluctuations, geologic events such as catastrophic floods, drainage-basin changes and isostatic rebound Reheis et al.

Several studies have been conducted to document the paleoenvironmental change on the TP by dating relict beach ridges and lacustrine sediments with optically stimulated luminescence OSL , cosmogenic radionuclides and 14 C methods e. Particularly, the OSL method has increasingly been applied to lacustrine deposits, owing to readily available dating materials, i. However, the problem of very dim natural and regenerative OSL signals from quartz samples has been reported in this region Long et al.

Several reconstructions of the past lake levels in the catchment of Selin Co Fig. Li et al. Those disagreements and uncertainties concerning the temporal patterns of past paleohydrological changes in this region could limit our understanding of the associated forcing mechanisms and the extent to which climate patterns could shift in response to future climate change Hou et al. Citation: Geochronometria ; In this paper, we carried out a combined stratigraphic and chronological analysis on a lacustrine outcrop from Cuoe Lake on the central TP.

Both luminescence and radiocarbon dating methods were used to reconstruct the evolution of the lake level during the Holocene.

Research Laboratory for Archaeology and the History of Art

Jain Mayank, Murray A. Optically stimulated luminescence dating: how significant is incomplete light exposure in fluvial environments? In: Quaternaire , vol.

the Oxford Luminescence Dating Laboratory. He holds a BSc(Hons) degree (​with distinction) in Geology from the University of Delhi ().

I took the opportunity and did an internship in the tephrochronology group at the University of Oxford. Description of the institution: The University of Oxford is the oldest university in the English-speaking world. Although there is no exact date of foundation, there is evidence for teaching activities since University of Oxford, a. Today, University of Oxford has more than students University of Oxford, b.

The university is organized into 38 colleges with Balliol-, Merton- and University College being the oldest ones, established between and These colleges can almost be seen as an independent university within the University of Oxford, because they are self-governing and financial independent. They are responsible for the selection and admission of undergraduate students and provide accommodation for them.

Graduate students apply directly to university but are selected by colleges after admission. Besides accommodation, the colleges provide facilities for catering and social and spiritual needs. Every college has a dining hall where breakfast, lunch and dinner are offered. Additionally, pretty much every college has its own library and chapel and its own sports classes.

Dr Matthew Telfer

Contact Professor Ian Bailiff email at ian. After reading physics at Sussex University Ian Bailiff joined the Research Laboratory for Archaeology and the History of Art at Oxford as a postgraduate student and subsequently submitted a research MSc on the development of new luminescence dating techniques. Following a further year working on an instrument development project he came to Durham in as a research assistant on a pottery dating project; following a series of appointments as a Research Fellow he was awarded an SERC Advanced Fellowship, and in was appointed a Lecturer.

He was Head of Department between and He has developed a luminescence dating laboratory with the capability to support both dating and methodological investigation, and his research has included the study of the luminescence properties of minerals, their application to dating and also to radiation dosimetry.

Scientists in North America first developed thermoluminescence dating of The Research Laboratory for Archaeology and the History of Art, Oxford University.

He acts as a reviewer for several international journals in the fields of environmental change, sustainability, applied physics, and has reviewed grants for various UK and international bodies. Richard’s current research interests are in the dynamics of natural environmental systems and coupled human-environment interactions over a range of timescales and contexts. The group works on understanding the dynamics of human, environmental, and coupled human-environmental systems, using mathematical modelling, numerical simulations, and empirical data analysis.

Many of the problems are theoretical, but the group also has a strong focus on applied projects – mostly on sustainability, and mostly in relation to ocean systems. The models created provide tools for all sorts for experimentation, and in the context of H-E systems are used alongside a variety of machine-learning methods for the development and exploration of implementable policies.

This work forms part of the Oxford Martin School Programme on Sustainable Oceans of which Richard is a co-Director , and uses a combination of theoretical modelling and empirical data analysis to investigate new practical approaches to fisheries management in a range of contexts. Finding management solutions which engender sustainability both ecologically and economically, in conditions which are dynamic and heterogeneous on a variety of temporal and spatial scales, is non-trivial and is the key problem that drives this research.

See here and here for further details. A combination of drivers is already influencing ocean biological communities, and the ecosystem services they provide, in significant ways. While habitat destruction and overfishing continue to top the list of critical near-term threats to the ocean, there is growing concern that changes in underlying ocean conditions e.

To supplement ongoing empirical work, there is a strong need for an effective analytical framework to quantify the effects of multiple stressors and to evaluate the consequences of interacting climate and non-climate stressors in marine systems. In response to these needs, Richard and his team have developed a new model framework OSIRIS – Ocean Systems Interactions, Risks, Instabilities and Synergies to help explore possible system-level consequences of multiple external environmental forcings.

Research interests

It was established in and its first director was Teddy Hall. Among the areas of research it has been involved in are:. From Wikipedia, the free encyclopedia. Among the areas of research it has been involved in are: Radiocarbon dating Luminescence dating Materials analysis Palaeodiet Archaeological geophysics Uranium-series dating Diagenesis The laboratory includes the Oxford Radiocarbon Accelerator Unit ORAU , which carries out radiocarbon dating using an accelerator mass spectrometer.

Research Laboratory for Archaeology and the History of Art. University of Oxford.

Luminescence Dating. Geochronology. Author’s address. ‘Research Laboratory for Archaeology and the History of Art, University of Oxford, 6 Keble Road.

To compare our experiment results with other laboratories by participating in international inter-laboratory comparison tests is an important need to ensure the accuracy of our measurements. However, so far, international comparison tests or measurements on OSL dating are unfortunately organized very limited in number. The latest inter-laboratory comparison study was conducted between and years by the Nordic Luminescence Laboratory in Denmark. For the calculation of annual dose rate Da , concentrations of radioactive isotopes U, Th, K were measured by using a high-purity germanium detector.

Consequently, within the error limits, we have determined the age of the sample close to the expected age. By participating in this comparison test, we have had the opportunity to compare our results with other luminescence dating laboratories and to ensure the accuracy of our results. At the same time, we had the chance to interpret each step of our dating measurements preparation of pure quartz minerals, determination of equivalent dose and annual dose etc. Turkish Journal of Nuclear Sciences contains scientific articles on nuclear and radiation issues.

Subject Coverage Keywords :. Activation Analysis. Atmospheric Distribution Calculations. Atomic and Molecular Physics.

Luminescence Dating

The Institute of geophysics of Tehran University is establishing a luminescence sample preparation laboratory. The following investigations and experiments was performed to find the safe light for this lab. This paper is written in Farsi to provide answer to many questions that the first author has been asked locally about which light is suitable for both sample preparation lab and in the field during sampling in dark. To answer those questions we decided to publish our finding.

Julie is a Supernumerary Teaching Fellow at St John’s College, Oxford and and the advancement of luminescence dating as a geochronological technique. Georgina is currently head of the Cologne Luminescence Laboratory at the.

Pleistocene human groups: cultures, evolutions and dynamics in Eurasia. After completing an initial M. Norbert Mercier and Dr. Christelle Lahaye. This research project focuses on the significant questions of the disappearance of Neanderthals from Eurasia, the associated spread of anatomically modern humans across Eurasia, and the extent to which there was contact with Denisovans in Siberia. As postdoctoral research fellow , I was responsible for the luminescence dating component of the project.

Since , I led a research project Oxford John Fell Fund which aims to develop a novel methodology for dating Plio-Pleistocene sediments, in order to provide numerical ages for major fossil and artefact-bearing sites in Africa. My approach is to apply a revolutionary luminescence-based method, I developed during my Ph. D, and known as infrared-radiofluorescence IR-RF to determine the age of sediments i. In September , I have been awarded a H. Early human evolution in Africa.

Early human dispersals into the Americas. Career path After completing an initial M.

Luminescence generation