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Magnetostratigraphy. Wout Krijgsman & Cor Langereis Paleomagnetic Laboratory Fort Hoofddijk Department of Earth Sciences Utrecht University. Magnetostratigraphy Possibilities, pitfalls and applications. Cor Langereis, Wout Krijgsman Paleomagnetic Laboratory Fort Hoofddijk
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Magnetostratigraphy Wout Krijgsman & Cor Langereis Paleomagnetic Laboratory Fort Hoofddijk Department of Earth Sciences Utrecht University
MagnetostratigraphyPossibilities, pitfalls and applications Cor Langereis, Wout Krijgsman Paleomagnetic Laboratory Fort Hoofddijk Dept. of Earth Sciences, Utrecht University Giovanni Muttoni Dept. of Earth Sciences, University of Milan Manfred Menning Geoforschungs Zentrum Potsdam, Germany
Mantle Convection time scale ~100 Myr Reversal frequency, superchrons Liquid outer core Convection time scale 300-500 yr Geodynamo action: Secular variation, excursions, reversals Solid inner core Diffusion time scale 3-5 kyr Stabilises geodynamo process Kuang & Bloxham, 1997 Origin of reversals
Lavas & K/Ar dating Sediments (DSDP) & biostratigraphy ? Marine magnetic anomalies GPTS: Geomagnetic Polarity Time Scale Barcode: may give unique solutions - but of an essentially BINARY nature - and can be distorted in the rock record
Magnetostratigraphy part of integrated stratigraphy Biostratigraphy: first-order chronology - taxonomy, reworking, diachrony, ages Magnetostratigraphy: globally synchonous barcode - depends on good paleomagnetic signal & recording Cyclostratigraphy: astronomical dating, fine-tuning - astronomical solutions (> 20 Ma) - interpretation of phase relations
Integrated stratigraphy Biostratigraphy - first-order chronology Magnetostratigraphy - globally synchonous barcode Cyclostratigraphy - fine-tuning & astronomical dating
Magneto-bio-stratigraphy Opdyke et al., 1966 - Advent of deep-sea cores: inclination only - Biostratigraphy (faunal zones) for dating
MarineMagneticAnomalies DeepSeaCores vs.
PaleomagnetismDRM vs. CRM:- inclination error- delayed NRM acquisition
Accuracy of recording reversals Watkins, 1968
Geomagnetic Polarity Time Scale(GPTS)or … Polarity zones (subchrons) or excursions (cryptochrons) ? Geomagnetic Instability Time Scale(GITS)‘reversal excursions’
Magnetostratigraphic resolution Laj & Channell (2007) proposed: Resolution depends on: - sampling resolution (easy … just take more samples) - sediments: sedimentation rate & suitable recording medium - diagenesis, lock-in depth, overprints, etc., etc.
Magnetostratigraphic resolution Nomenclature OK … but for practical (integrated) stratigraphy and constraints on chronostratigraphy ?
Marine magnetic anomalies World crustal age
The times they are a-changin’ (Bob Dylan, 1964) Wout Krijgsman
Time: dates and rates Tools: Biostratigraphy Magnetostratigraphy Astrochronology Isotopic dating Aims: Marine-continental Paratethys-Mediterranean Synchrony-diachrony Event stratigraphy
Geological Time ScaleGradstein et al. (2004)GTS2004 Neogene: based on astronomical ages Paleogene: based on radio-isotopic ages
Magnetostratigraphy & Cyclostratigraphy Astronomical TuningClimate cyclesAstronomical solutions Hilgen et al., 2004
Astronomical Polarity Time Scale (APTS) for the Mediterranean Neogene
Sampling, 15 years ago Sicily, 2 weeks ago
Accurate definition of GSSP (Oued Akrech, Hilgen et al., 2000) Cyclostratigraphy & astronomical tuning ... ATNTSin GTS2004 Lourens et al., 2004
Biostratigraphy vs. Magnetostratigraphy • Problems: • Taxonomy • Diachrony • Reworking • Ages • Problems: • Correlation • Primary signal • vs. overprint • Ages
Correlation Requires unique pattern fit Magneto age 7.6 ± 0.1 K/Ar age 6.16 ± 0.30 Garces et al., 2001
Ages GPTS not independent of other dating techniques
The times they are a-changing’ Ages change with time …
Astrochronology • Problems: • Cycle recognition • Phase relation • Correlation • Astronomical solution
Astrochronology: correlation of cyclic variations in the geological record to computed astronomical (age) curves
Sapropel-marl cycles, upper Miocene, Sicily Eccentricity minimum Precession minimum Gibliscemi, Sicily, Italy
Partial Unit-Stratotype of the Zanclean stage (Lower Pliocene) Punta di Maiata, Sicily, Italy
Lignite-marls cycles, Mio-Pliocene, Greece Precession minimum Ptolemais quarry, Greece
Sand-marls cycles, Mio-Pliocene, Romania PONTIAN Acc. rate in C3r = 137cm/kyr Periodicity cycles = 22.7kyr Putna river section,eastern Carpathians
Clay-carbonate cycles, Miocene, Spain Orera section, Spain
Clay-carbonate cycles, Triassic, USA Painted desert/Petrified forrest, Arizona
MioceneAPTS • Astrochronology for the Late Miocene • Sections on Crete correlated bed-to-bed to Sicily Hilgen et al. (1995)
Messinian evaporites Northern Apennines (Italy)