University of Georgia

In the sciences, it is important to distinguish between precision and accuracy. If we use the analogue of a clock we can investigate this further. Your wrist watch may measure time with a precision of one second. A stop watch may time your race with a precision of one hundredth of a second. However, if the clocks change and you forget to reset your wrist watch, then you have a very precise time but it is not very accurate — you will be an hour early or late for all of your meetings! Scientists want measurements that are both accurate and precise… but it can be difficult to tell sometimes whether very precise measurements are actually accurate without an independent reference age see top right image versus bottom right image. Accurate measurements fall in the bulls eye.

Optically stimulated luminescence

HOW-TO SERIES Luminescence dating provides a direct age estimate of the time of last exposure of quartz or feldspar minerals to light or heat and has been successfully applied to deposits, rock surfaces, and fired materials in a number of Sampling strategies are diverse and can be customized depending on local circumstances, although all sediment samples need to include a light-safe sample and material for dose-rate determination.

The accuracy and precision of luminescence dating results are directly related to the type and quality of the material sampled and sample collection methods in the field.

They say that the ‘dating of the ash is complicated by the fact that an eruption occurred underwater.’ The team reanalyzed the tuff by optically stimulated luminescence (OSL), a method that requires sampling deep within the tuff and in complete darkness.

Results Strandlines The number of mappable or resolvable strandlines was controlled by the resolution of the available basemap or DEM data set. Many strandlines are evident on orthophotography and soil survey maps. On steeper slopes, strandlines are represented by scarps that often pass laterally into ridges where locally slopes lessen or the aspect changes. Results are reported using the sampling elevation as the label for the strandline.

Often there are clusters of strandlines associated by elevation or distribution with the sampled strandlines. In all but one case KG , the sampled strandline is the most prominent in the group. Strandline grouping is presented from highest to lowest elevation. The muted topography and poorly developed strandlines are presumed to have resulted from short-lived levels of proglacial lakes trapped between higher topography to the west and the retreating ice margin to the east until larger fetches developed following retreat of the glacier margin.

Below this group is a well-developed scarp on the north of Fig. Below this ridge is a flight of up to 10 very-low-relief ridges. Farther north, there is another flight of strandlines at the same elevation as the ridge flight just mentioned. To the east and below the elevation of both flights of strandlines is a nearly continuous strandline that transitions laterally between scarps, ridges, and spits.

Here intermediate elevation strandlines are absent Fig.

USU OSL Laboratory

Stright, Lear, and Bennett A chipped-stone projectile point lies amid broken shell and other beach detritus washed onshore. Photo by David Crain.

Optically Stimulated Luminescence (OSL) Dating Sediment samples from all 11 terrestrial vibracores were collected for optically stimulated luminescence (OSL) dating. Care was taken not to expose the sediment to light, and all sampling was conducted in the dark with only a photographer’s red lamp; however, six of the cores were split into 1-m lengths before sampling.

How do we measure the radiation dose rate? OSL is used on glacial landforms that contain sand, such as sandur or sediments in glacial streams. The OSL signal is reset by exposure to sunlight, so the signal is reset to zero while the sand is being transported such as in a glacial meltwater stream. Once the sand grain has been buried and it is no longer exposed to sunlight, the OSL signal starts to accumulate.

OSL works because all sediments have some natural radioactivity, caused by the presence of uranium, thorium and potassium isotopes in heavy minerals such as zircons. We analyse the quartz or feldspar minerals in sand deposits. When these quartz or feldspar minerals are exposed to the ionising radiation emitted by the radioactive isotopes in zircons, electrons within the crystals migrate and become trapped in their crystal structure.

The number of trapped electrons depends on the total amount of radiation that the mineral has been exposed to. If we assume that the radiation dose rate of the sediment has remained constant over time, then if we measure that dose rate, we can calculate the sample age. How do we measure the OSL signal? Photograph used with permission of Geoff Duller.

The way that we do this is through sampling sand from the landforms in opaque plastic tubes and taking the sample back to a luminescence laboratory where only red light conditions are used. We have to be very careful not to expose the sediments to sunlight when we do this! It is necessary to use red light conditions in the laboratory because the luminescence signal is light sensitive, and red light does not re-set it.

Department of Geosciences

Can we unravel preservation and sampling bias from climatic depositional overprints? Samples have been collected from fluvial deposits that constitute terraced valleys, alluvial plains and terrestrial basin fills, using various strategies shallow outcrops, deeper quarries, high quality cores The former area hosts a terraced fluvial sequence with low valley gradients developed in older Plio-Pleistocene alluvium, the latter area a stacked basin-fill with even lower valley slope.

Over the full length of the region the Rhine river was in braided mode during Pleistocene glacial maxima and in meandering mode during interglacials. Glacial-interglacial transitions lead to geomorphological adaptations along the Lower Rhine valley, lastly between 15, and 8, years ago.

Optically stimulated luminescence (OSL) dating is a method of absolute geochronology that has been widely applied in Quaternary studies since its proposition by Huntley () and further development of the Single-Aliquot Regenerative Dose (SAR) protocol by Banerjee et al. () and Murray and Wintle (). The SAR dating protocol is now the.

Optically-Stimulated Luminescence is a late Quaternary dating technique used to date the last time quartz sediment was exposed to light. As sediment is transported by wind, water, or ice, it is exposed to sunlight and zeroed of any previous luminescence signal. Once this sediment is deposited and subsequently buried, it is removed from light and is exposed to low levels of natural radiation in the surrounding sediment.

Through geologic time, quartz minerals accumulate a luminescence signal as ionizing radiation excites electrons within parent nuclei in the crystal lattice. A certain percent of the freed electrons become trapped in defects or holes in the crystal lattice of the quartz sand grain referred to as luminescent centers and accumulate over time Aitken, In our laboratory, these sediments are exposed to an external stimulus blue-green light and the trapped electrons are released.

The released electrons emit a photon of light upon recombination at a similar site. In order to relate the luminescence given off by the sample to an age, we first need to obtain the dose equivalent to the burial dose. Following the single-aliquot regenerative SAR method of Murray and Wintle , the dose equivalent De is calculated by first measuring the natural luminescence of a sample. Then, the bleached sample is given known laboratory doses of radiation, referred to as regenerative doses.

The regenerative dose data are fit with a saturating exponential to generate a luminescence dose-response curve.

Dr Julie Durcan

Post-processing of the sidescan sonar data will allow plans of the areas of exposed peat to be input into the GIS database. The sidescan images will also be mosaiced to form a continuous image of the seabed surface. Palaeoenvironmental Sampling In the first year of field work the mapping and sampling of inter-tidal peats will be carried out during the lowest tides and will use existing data as a starting point to confirm areas of peat and to establish their hieght above ordanance datum.

An initial assessment of the quality and quantity of material available at the potential inter-tidal sampling locations will be made. The initial results of offshore survey will be used to identify a test site for offshore peat sampling. Various techniques for land and sea-based sampling will be tested.

OSL dating of sediments associated with Paleoindian archaeology (Holliday et al. OSL ages of upper Quaternary eolian sand and paleosols, northwest Albuquerque Basin, New Mexico Stephen A. Hall, sampling, the material was discarded and a.

The ancient copper mines of Timna Valley have been the subject of systematic research for the past 40 years led by Beno Rothenberg. As human activity in mines leaves scant remains of material culture i. Rothenberg and the Arabah Expedition were the first to systematically excavate and identify three types of mining technology in Timna Valley. Mining Technologies Type A: These sandstone cliffs contain copper ore deposits, which have eroded and deposited the copper ore nodules into the silt and gravel conglomerate valleys over time.

It is difficult to distinguish these types of mines Figure 1; Merkavot 1 because they look like typical surface erosion in the valleys. However, the depressions on the surface represent ancient open-pit mining practice. When the miners extracted the copper ore nodules, they left shallow pits and over time are refilled with dust, silt and rocks that leave the even more shallow in the present day.

Due to the simple nature of this mining technology, it has long been associated with the chalcolithic period.

The Grotte Mandrin

Archaeology , dating , footprint , mexico , optically stimulated luminescence , peopling of the americas , toloquilla , valsequillo basin The peopling of the Americas is one of my favorite subjects in anthropology. These footprints were within a soft, damp volcanic ash along a lakeshore shortly after a volcanic eruption. This type of volcanic tuff is known as the Xalnene.

Samples of the Xalnene tuff were sent off to the Berkeley Geochronology Center for argon-argon and paleomagnetic dating. The team that initially found the prints have revisited the dating of the Xalnene tuff at Toloquilla.

The OSL field sampling (Figure 10) and processing was conducted under the guidance of Dr. Naomi Porat and Galina Faershtein in collaboration with Craig Smitheram and the CTV team. Our results from the excavated mines provide a reliable anchor for dating ancient mines.

These currently include geomorphology, biogeography, climatology and Quaternary Science, but are subject to change in response to the department syllabi. I also teach lectures in the School of Geography and Environment. Research Interests My research focuses on the reconstruction of climate and environment over the past 2. I mainly focus on dryland regions, and am most interested in the interaction between ancient civilisations and climate change over the past 10, years.

My current research projects include: Examining river activity over the past 10, years in northwest India to understand the relationship between changing hydrology and civilisation collapse. Understanding the relationship between changing lake levels and ancient human activities in the Thar Desert, India over the past , years. Development of the sediment dating technique luminescence dating. Selected Publications Srivastava, A.

Holocene dune activity in the Thar Desert, India.

Precision and accuracy in glacial geology

The application of the method to fossil teeth requires the collection of a number of data related to the geological environment of the sample e. During the burial of a tooth, the production of radiations from U, U from the surrounding sediment and within the tooth, which incorporates U during fossilization , Th decay chains and 40K from the surrounding sediment , as well as cosmic rays damage the hydroxyapatite structure of the tooth enamel fig.

In contrast, the dose rate is evaluated by measuring the radioactivity in the tooth itself in all the dental tissues constituting the tooth, i. Equid teeth are also appropriate, although it should be taken into account that the porosity of the cement covering the external side of the enamel can lead to some issues regarding U-uptake modelling. If these species are lacking from the faunal assemblage, smaller teeth, from species such as cervid and ovicaprid, can be collected, whereas carnivora teeth are usually not recommended, given their thin enamel layer; 8— the selected tooth should preferentially be well preserved, as previous studies show a direct correlation between fractures and diagenetic weaknesses in dental tissues and preferential migration of U-series elements e.

This is a problem we regularly encounter in chronostratigraphy. Analytical techniques are very advanced and precise, but they may be inaccurate.

Because of minimal subglacial erosion, bedrock surfaces may have an inherited component of cosmogenic nuclides and the total concentration will represent a composite signal. This can be avoided by using two cosmogenic nuclides with significant different half-lives e. However, this requires both long exposure periods prior to glacial overriding and long duration of subsequent burial, in order to detect exposure discontinuities.

To circumvent this, we combine single nuclide exposure dating 10Be and optically stimulated luminescence OSL dating in sample settings that include contemporaneous erosion and deposition. By using this multiple dating method approach, we expect to obtain reliable exposure age estimates and also to be able to identify burial by cold-based ice. The field area in east-central southern Norway has numerous OSL dated sedimentary deposits ranging in age from the present to ka, often with evidence of glacial overriding e.

Such deposits are commonly connected to lateral meltwater channels, glaciofluvially washed valley slopes, overflow gaps and canyons, all which have the potential to have been sufficiently eroded to remove previously accumulated cosmogenic isotopes. Three scenarios can be envisaged when comparing exposure and OSL ages from our time-synchronous sampling settings:

OTHER DATING TECHNIQUES

The luminescence dating facilities consist of three purpose-built laboratories: The sample preparation facility is fully equipped with all the necessary equipment to obtain pure quartz, feldspar and polymineral fine-grain fractions from bulk sediment sa The sample preparation facility is fully equipped with all the necessary equipment to obtain pure quartz, feldspar and polymineral fine-grain fractions from bulk sediment samples. Laboratory equipment includes two fume hoods with scrubbers for HF etching and other chemical treatments, ovens, automated sieve-shaker, Frantz magnetic separator, ultrasonic bath, centrifuge, Millipore system, weighing scales, binocular microscopes, and single-grain and multi-grain aliquot preparation facilities.

One of the readers is also equipped with a combined blue and IR pulsed optical stimulation unit and photon timer attachment. For field-based dose rate evaluation, we are equipped with portable gamma spectrometers and in situ dosimeters.

Background. Initially identified in , excavation at Area 15 of the Gault Site was undertaken to explore evidence of early cultures in Central ch focused on the manufacturing technologies, their relationship to Clovis, and the associated age of this assemblage.

A Twa hunter-gatherer in Uganda climbing a tree to gather honey. Nathaniel Dominy Early Human Ancestors May Have Walked AND Climbed for a Living Africa 31 December The results of recently conducted field studies on modern human groups in the Philippines and Africa are suggesting that humans, among the primates, are not so unique to walking upright as previously thought. The findings have implications for some of our earliest possible ancestors, including the 3. Associate professor of anthropology Nathaniel Dominy of Dartmouth College, along with colleagues Vivek Venkataraman and Thomas Kraft, compared African Twa hunter-gatherers to agriculturalists living nearby, the Bakiga, in Uganda.

In the Philippines, they compared the Agta hunter-gatherers to the Manobo agriculturalists. They found that the Twa and the Agta hunter-gatherers regularly climbed trees to gather honey, an important element in their diets. More specifically, they observed that the climbers “walked” up small trees by applying the soles of their feet directly to the trunk and progressing upward, with arms and legs advancing alternately.

To do this successfully, they said, required extreme dorsiflexion, or bending the foot upward toward the shin to a degree not normally possible among most modern humans. They tested their hypothesis by conducting ultrasound imaging of the fibers of the large calf muscles of individuals in all four groups. The results showed that the Agta and Twa tree-climbers had significantly longer muscle fibers than those of their agricultural counterparts and other “industrialized” modern humans.

It demonstrated that a foot and ankle bone structure adapted primarily for walking upright on land does not necessarily exclude climbing as a behaviorally habitual means of mobility for survival. The implications for our possible early human ancestors, such as the species Australopithecus afarensis, are significant. Australopithecus afarensis is an extinct hominid that lived between 3.

CRAN Packages By Name

Our reports contain official radiocarbon dating certificates for each sample together with calibration curves showing how each conventional radiocarbon age for samples has been calibrated with the calendar year curve. Application Suitable for dating sediments up to c. Non-marine as well as marine and terrestrial sediments can be dated using this method.

Each sample is prepared in the same way as for a micropalaeontological analysis. Suitable specimens are selected by picking through the residue.

Optically stimulated luminescence dating of sandy deposits from Gulang county at the southern margin In contrast, the optically stimulated luminescence (OSL) dating technique determines the elapsed time since the last instance of exposure to sunlight or the last time that deposition occurred. The rectangles denote the sampling sections.

However, arroyo response to climate change is still not well understood. Many geomorphic studies indicate that minor climate shifts can cause major perturbations to streams in the southwestern U. Ely ; Hereford ; Vivoni et al, Given climate model predictions for the SW U. The headwaters of the Escalante River in S. Utah provide an excellent setting to examine the timing of arroyo cycles in relation to climate change.

Greg Balco – Cosmogenic-Nuclide Geochronology