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Description
  • Geology and palaeontology of the Roudníky area, situated between the Most Basin and the České středohoří Mountains in North Bohemia, the Czech Republic, is treated in detail. The volcano-sedimentary structure underlying the basin with the included fossiliferous layers is newly interpreted as a maar-diatreme. The radiometric age of the basalts was determined to 35.4 +- 0.9 Ma and 37.1 +- 0.9 Ma - late Eocene, Priabonian. The fish fauna consists of amiids characteristic of other adjacent late Eocene sites while the co-occurring macroflora includes many elements that are typical of the Oligocene. Closest relations are to the fauna and flora of the Větruše Hill at Ústí nad Labem. Based on palaeoclimatic estimates the major turnover from subtropical to warm-temperate climatic regimes in North Bohemia appears to have initiated in the late Eocene by an increase of seasonality and the resulting vegetation change from the evergreen to mixed mesophytic forest types well before the maximum temperature drop of mean annual temperature at ca 33.5 Ma.
  • Geology and palaeontology of the Roudníky area, situated between the Most Basin and the České středohoří Mountains in North Bohemia, the Czech Republic, is treated in detail. The volcano-sedimentary structure underlying the basin with the included fossiliferous layers is newly interpreted as a maar-diatreme. The radiometric age of the basalts was determined to 35.4 +- 0.9 Ma and 37.1 +- 0.9 Ma - late Eocene, Priabonian. The fish fauna consists of amiids characteristic of other adjacent late Eocene sites while the co-occurring macroflora includes many elements that are typical of the Oligocene. Closest relations are to the fauna and flora of the Větruše Hill at Ústí nad Labem. Based on palaeoclimatic estimates the major turnover from subtropical to warm-temperate climatic regimes in North Bohemia appears to have initiated in the late Eocene by an increase of seasonality and the resulting vegetation change from the evergreen to mixed mesophytic forest types well before the maximum temperature drop of mean annual temperature at ca 33.5 Ma. (en)
Title
  • Tracing the Eocene-Oligocene transition: a case study from North Bohemia
  • Tracing the Eocene-Oligocene transition: a case study from North Bohemia (en)
skos:prefLabel
  • Tracing the Eocene-Oligocene transition: a case study from North Bohemia
  • Tracing the Eocene-Oligocene transition: a case study from North Bohemia (en)
skos:notation
  • RIV/00216208:11310/14:10283159!RIV15-MSM-11310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(GA14-23108S), P(GAP210/10/0124), Z(MSM 113100006), Z(MSM0021620855)
http://linked.open...iv/cisloPeriodika
  • 1
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 50892
http://linked.open...ai/riv/idVysledku
  • RIV/00216208:11310/14:10283159
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • boundary; early Oligocene; late Eocene; vegetation; climate; fauna; flora (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [55438F3302DA]
http://linked.open...i/riv/nazevZdroje
  • Bulletin of Geosciences
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 89
http://linked.open...iv/tvurceVysledku
  • Dvořák, Zdeněk
  • Kvaček, Zlatko
  • Mach, Karel
  • Teodoridis, Vasilis
  • Přikryl, Tomáš
http://linked.open...ain/vavai/riv/wos
  • 000330188000002
http://linked.open...n/vavai/riv/zamer
issn
  • 1214-1119
number of pages
http://bibframe.org/vocab/doi
  • 10.3140/bull.geosci.1411
http://localhost/t...ganizacniJednotka
  • 11310
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