Geochronological accuracy around the cretaceous paleogene boundary interval insights and challenges to the age of chron C29r and intervening events

2015-07-02
Yılmaz, İsmail Ömer
Stoykova, Kristina
The need for precise and accurate time constraints in Earth sciences is pivotal to successfully unravel geological mechanisms and rates of processes. Timescale accuracy is a prerequisite for reliable event correlation and to disentangle intricate complex climatic and biotic changes. The late Cretaceous, a time interval of major biodiversity adjustments culminating in the end-Cretaceous mass extinction, has been the subject of intense debates regarding not only its causes but also the timing. The Cretaceous-Paleogene (K-Pg) boundary occurs within Chron C29r. Its numerical age and the relative position within C29r has changed significantly over different instances of the GPTS. The radiometric absolute age of the K-Pg boundary has now been established at 66.043 ± 0.043 Ma by high-precision 40 Ar/ 39 Ar dating on tektites and bentonites associated with the boundary. The age close to 66 Ma is compatible with astronomical tuned chronologies derived from integrated magneto/chemo/biostratigraphic studies from marine sequences that have provided complete orbital chronologies for the Maastrichtian and Paleocene at eccentricity resolution (~100-400 ky). These studies also place the K-Pg halfway C29r with a calibrated Chron duration of ~710 ky. However, a recent chronostratigraphic study of the terrestrial K-Pg transition in the Hell Creek region (Montana) including 40 Ar/ 39 Ar dating of 15 tephra layers challenge the duration of C29r to as brief as ~345 ky. Here, the chronological framework of C29r is reappraised and studied at orbital precession resolution (~21 ky) using an array of deep sea records and new data from pelagic strata from the Bjala section (Bulgaria) and the Mudurnu-Goynuk basin (NW Turkey).
26th IUGG, (22 Haziran - 02 Temmuz 2015)

Suggestions

Tectonic and thermal evolution of a Metamorphic Core Complex: the Menderes Massif (Western Turkey)
Bozkurt, Erdin (null; 2018-04-08)
Understanding the origin of lithospheric- and crustal-scale thermal anomalies requires the study of the long-term thermo-tectonic evolution at large spatial-temporal scales. For instance, cold plate-converging settings (i.e. involving subduction) may exhume first colder units still preserving HP-LT assemblages from the earlier nappe stack, and then HT-LP parageneses in the post-orogenic setting. In both cases, the thermal evolution of such assemblages depends primarily on whether the basement is involved in...
Sedimentary basin deformation: an incremental stress approach
Tuncay, Kağan; Ortoleva, P. (Elsevier BV, 2000-8)
A key component of sedimentary basin evolution is the spatial distribution and temporal variation of stress and deformation. The many deformation processes (poroelasticity, fracturing, irreversible nonlinear viscosity, and pressure solution) are inextricably bound in a tightly coupled network which, in turn, is coupled to a myriad of basin diagenetic, thermal and hydrologic processes. In the approach presented here, the various deformation processes are integrated through an incremental stress approach. Tog...
Uncertainty quantification by using stochastic approach in pore volume calculation for geothermal reservoir
Gürel, Emrah; Akın, Serhat; Department of Petroleum and Natural Gas Engineering (2015)
This study will present the application of a stochastic approach and experimental design techniques to a geologic system in order to quantify the uncertainty of pore volume estimations for a liquid dominated high temperature geothermal reservoir. The pore volume is a key element when defining the total resource available in the field. Alasehir geothermal reservoir pore volume uncertainty has been assessed. The uncertainties being addressed include geometry (top of reservoir and base of reservoir), reservoir...
Estimating tectonic history through basin simulation-enhanced seismic inversion: geoinfomatics for sedimentary basins
Tandon, K; Tuncay, Kağan; Hubbard, K; Comer, J; Ortoleva, P (Oxford University Press (OUP), 2004-01-01)
A data assimilation approach is demonstrated whereby seismic inversion is both automated and enhanced using a comprehensive numerical sedimentary basin simulator to study the physics and chemistry of sedimentary basin processes in response to geothermal gradient in much greater detail than previously attempted. The approach not only reduces costs by integrating the basin analysis and seismic inversion activities to understand the sedimentary basin evolution with respect to geodynamic parameters- but the tec...
Geotechnical characterization and rock mass classification of the Antalya karstic rock masses
Sopacı, Evrim; Akgün, Haluk; Department of Geological Engineering (2012)
This thesis identifies the geotechnical parameters of the Antalya karstic foundation rocks (travertine/tufa), which are highly variable in nature, by means of geological observations, geotechnical site investigations, and field and laboratory geomechanics tests to examine karstic (mainly tufa) rock mass behavior. Several geotechnical parameters such as porosity, seismic wave velocity, uniaxial compressive strength, Young’s modulus, tensile strength, etc. that are thought to have significant influence on roc...
Citation Formats
İ. Ö. Yılmaz and K. Stoykova, “Geochronological accuracy around the cretaceous paleogene boundary interval insights and challenges to the age of chron C29r and intervening events,” Prag, Çek Cumhuriyeti, 2015, p. 3042, Accessed: 00, 2021. [Online]. Available: http://www.iugg2015prague.com/.