Paleomagnetic analyses on Badenian–Sarmatian drill cores from the North Carpathian Foredeep (Middle Miocene, Poland)

Journal Title: Biuletyn Państwowego Instytutu Geologicznego - Year 2015, Vol 461, Issue 461

Abstract

Accurate dating of the Badenian–Sarmatian transition, a boundary between two regional Middle Miocene stages of the semi-isolated Paratethys Sea, is crucial to understand what event caused the corresponding major turnover in faunal assemblage at that point in time. The general opinion is that this event resulted from a sudden isolation of the Eastern Paratethys from ocean water, due to the closure of the Eastern Anatolian seaway to the Indian Ocean, but it remains debated if the final isolation had a tectonic or climatic cause. This pilot study presents paleomagnetic analyses of two drill cores from the North Carpathian Foredeep in Poland that straddle the Badenian–Sarmatian transition. Rock magnetic experiments, including thermomagnetic runs in air on a Curie balance, and hysteresis measurements on a MicroMag, indicate that the dominant magnetic carrier is the iron sulphide greigite. This is in agreement with the observed gyroremanence obtained during alternating field demagnetization above 40 mT. Alternating field and thermal demagnetization results are in good agreement and show a weak, mixed-polarity, signal for most of the Badenian, rapidly shifting to a much stronger and dominantly normal polarity signal in the Sarmatian part of the cores. First order reversal curves diagrams indicate that the greigite in the Sarmatian part is clearly of diagenetic origin, it thus most likely concerns a secondary overprint by the present-day field that cannot be used for magnetostratigraphic correlations. We conclude that the Paratethys-wide paleoenvironmental change that occurred at the Badenian–Sarmatian transition had probably also created different conditions for the formation and/or preservation of magnetic minerals.

Authors and Affiliations

Karin SANT, Arjan de LEEUW, Liao CHANG, Andrzej GĄSIEWICZ, Grzegorz Czapowski, Wout KRIJGSMAN

Keywords

Related Articles

INFILTRATION CAPACITY OF WEATHERING RESIDUALS IN GNEISES OF WIELKA SOWA MASSIF (MIDDLE SUDETES)

The paper presents the results of the hydrogeological investigations carried out in the Sowie Góry massif in order to estimate infiltration capacity of the weathering cover of gneisses. Based on fields works there were e...

POLLUTION OF SOIL-AQUATIC ENVIRONMENT BY HEAVY METALS IN THE OLD ALEXANDER SMELTER AREA IN KIELCE

In the protective zone of municipal groundwater intake, in the former industrial district named Białogon, which is the southern part of the city of Kielce, the metal industry has operated for about 200 years. The studies...

PRZEJAWY MINERALIZACJI KRUSZCOWEJ W SKAŁACH NAWIERCONYCH OTWORAMI TROJANOWICE 2 I CIANOWICE 2

Okruszcowanie w skałach ediakaru w otworze wiertniczym Cianowice 2 jest bardzo ubogie. Dość bogaty jest jednak zespół mineralny reprezentowany przez: chalkopiryt, piryt, piryt framboidalny, bornit, minerały szeregu galen...

MODELOWANIE HYDROGEOCHEMICZNE W BADANIACH KRĄŻENIA WÓD PODZIEMNYCH NA PRZYKŁADZIE SALARU ATACAMA, PÓŁNOCNE CHILE

Strefa kontaktu wód słodkich ze słonymi najlepiej rozpoznana została na wybrzeżach morskich, lecz występuje także w salarach wypełniających niecki endoreiczne. W pracy przedstawiono tylko część modelu hydrogeochemicznego...

APPLICATION OF NUMERICAL MODEL OF GROUNDWATER FLOW IN DESIGNING THE DRAINAGE WELLS BARRIER IN THE VICINITY OF THE INDUSTRIAL WASTE LANDFILL

This article presents practical application of numerical model of ground water flow in designing the drainage wells barrier and assessing its effectiveness in protecting groundwater in the vicinity of the industrial wast...

Download PDF file
  • EP ID EP63589
  • DOI -
  • Views 43
  • Downloads 0

How To Cite

Karin SANT, Arjan de LEEUW, Liao CHANG, Andrzej GĄSIEWICZ, Grzegorz Czapowski, Wout KRIJGSMAN (2015). Paleomagnetic analyses on Badenian–Sarmatian drill cores from the North Carpathian Foredeep (Middle Miocene, Poland). Biuletyn Państwowego Instytutu Geologicznego, 461(461), 179-192. https://europub.co.uk/articles/-A-63589