Global correlation of Upper Campanian - Maastrichtian successions using carbon-isotope stratigraphy: development of a new Maastrichtian timescale

Voigt, Silke; Gale, Andrew S.; Jung, Claudia; Jenkyns, Hugh C.

doi:10.1127/0078-0421/2012/0016

Cited by 161 publications

(155 citation statements)

References 104 publications

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“…Jung et al (2012) show many small δ 13 C peaks during the CMBE and extended the CMBE to the T. radiosus Zone (see also Voigt et al 2012). Voigt et al (2012) connect the CMBE with global tectonic movements rather than climate cooling. In these terms, the upper horizon from Strzeżów Pierwszy 1 could be a result of a short-term sea-level pulse.…”

Section: Global Sea-level Changesmentioning

confidence: 92%

“…redbirdensis to E. typica Zones (Ogg and Hinnov 2012). Jung et al (2012) show many small δ 13 C peaks during the CMBE and extended the CMBE to the T. radiosus Zone (see also Voigt et al 2012). Voigt et al (2012) connect the CMBE with global tectonic movements rather than climate cooling.…”

Section: Global Sea-level Changesmentioning

confidence: 95%

“…), gastropods and large sponges were reported. This horizon, which is an effect of slower or absence of sedimentation, could be connected with the Late Campanian Event (LCE) described by Voigt et al (2012) from France, England, Italy and Germany (Niebuhr et al 2011), which is manifested by a negative δ 13 C excursion. In Tercis (France), the LCE was recognized between the interval without any ammonite and inoceramid documentation and the 'I.'…”

Section: Global Sea-level Changesmentioning

confidence: 98%

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Inoceramid stratigraphy and depositional architecture of the Campanian and Maastrichtian of the Miechów Synclinorium (southern Poland)

Jurkowska¹

2016

Acta Geologica Polonica

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Dynamic evolution of the Campanian and Maastrichtian (Upper Cretaceous) of the Miechow Synclinorium is presented. Through chronostratigraphic analysis, the geometry of the Campanian and Maastrichtian of the area is interpreted, while microfacies analysis allowed determination of some of the paleoenvironmental parameters (rate of sedimentation, bottom condition and terrigenous input). The chronostratigraphy is based on inoceramid biostratigraphy. Nine inoceramid zones are recognized: Sphenoceramus patootensiformis, Sphaeroceramus sarumensis-Cataceramus dariensis and ‘Inoceramus’ azerbaydjanensis-‘Inoceramus’ vorhelmensis, ‘Inoceramus’ tenuilineatus, Sphaeroceramus pertenuiformis, ‘Inoceramus’ inkermanensis and ‘Inoceramus’ costaecus- ‘Inoceramus’ redbirdensis (Campanian); Endocostea typica and Trochoceramus radiosus (Maastrichtian). Five unconformities (isochronous in the study area) represented by horizons of slower sedimentation rate, were recognized. They correlate with eustatic sea-level changes, well recorded in European successions (Jarvis et al. 2002, 2006; Niebuhr et al. 2011). Unconformity horizons allow six alloformations to be distinguished. The thickness of particular chronostratigraphic units within the Campanian and Lower Maastrichtian increases progressively toward the axis of the Danish-Polish Trough, which indicates that the inversion of the trough could not have started before the Late Maastrichtian.

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Section: Global Sea-level Changesmentioning

confidence: 92%

Section: Global Sea-level Changesmentioning

confidence: 95%

Section: Global Sea-level Changesmentioning

confidence: 98%

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Inoceramid stratigraphy and depositional architecture of the Campanian and Maastrichtian of the Miechów Synclinorium (southern Poland)

Jurkowska¹

2016

Acta Geologica Polonica

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“…The CampanianeMaastrichtian boundary event is a significant interval in global environmental change, as observed in the oceanic record (see Jung, Voigt, & Oliver, 2012;Voigt, Gale, Jung, & Jenkyns, 2012) that was characterized by climatic cooling and sea-level fall. Here, we study the regression that took place around the CampanianeMaastrichtian boundary in the Southern Pyrenees (northeastern Iberia, Ibero-Armorican domain), when fully marine palaeo-environments were replaced by the transitional and continental.…”

Section: Introductionmentioning

confidence: 99%

Transitional environments of the lower Maastrichtian South-Pyrenean Basin (Catalonia, Spain): The Fumanya Member tidal flat

Oms

Fondevilla

Riera

et al. 2016

Cretaceous Research

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“…Note slightly increased palaeotemperatures of belemnites from the Misburg Formation (left segment) and the conspicuous latest Campanian cooling event which is evident in both datasets. Campanian-Maastrichtian boundary age after Ogg and Hinnov (2012) and Voigt et al (2012).…”

Section: Belemnite Palaeobiology and Water Mass Characteristicsmentioning

confidence: 99%

High-resolution Campanian–Maastrichtian carbon and oxygen stable isotopes of bulk-rock and skeletal components: palaeoceanographic and palaeoenvironmental implications for the Boreal shelf sea

Wilmsen¹,

Niebuhr²

2017

Acta Geologica Polonica

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ABSTRACT:Wilmsen, M. and Niebuhr, B. 2017. High-resolution Campanian-Maastrichtian carbon and oxygen stable isotopes of bulk-rock and skeletal components: palaeoceanographic and palaeoenvironmental implications for the Boreal shelf sea. Acta Geologica Polonica, 67 (1), 47-74. Warszawa.A high-resolution latest Early Campanian to Early Maastrichtian carbon and oxygen stable isotope record from the northern German Boreal shelf sea based on 537 analyses of co-occurring belemnites, brachiopods, inoceramids, oysters, and bulk rock samples is presented. All samples are precisely related to their stratigraphic, systematic and facies backgrounds and form an integrated, nearly 10-myr-long dataset with considerable palaeoenvironmental and palaeoceanographical implications. Petrographic studies indicate that low-magnesium calcitic coccoliths and calcispheres (i.e., planktic carbonate) predominate the bulk-rock data (marl-limestone rhythmites and chalks), thus representing a sea-surface water signal, and that only minor diagenetic alteration of the carbonate muds took place. Based on TL and CL microscopy, the investigated belemnites are extraordinarily well preserved, which may in part be explained by their early diagenetic surficial silicification (container effect), while the other macroinvertebrate groups are all less well preserved. The (plankton-dominated) d O signal of ambient seawater (12 ± 2°C). In the absence of any indication for migration from cooler water masses and evidence for authochtonous populations we assume that the belemnites of the genera Belemnitella and Belemnella lived as nektobenthos near the sea-floor and thus record the temperature of the bottom mixed layer of the seasonally weakly stratified north German shelf sea at water depths of 100 to 150 m; the temperature gradient was thus 12.5-18.75 m/1°C. A conspicuous latest Campanian cooling event is evident in both sea-surface and bottom-water temperatures. The d 18O values of nearly all investigated benthic fossils lie between the isotope values of pristine belemnites and bulk rock, and, therefore, should be used for palaeotemperature reconstructions only with great care.

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Global correlation of Upper Campanian - Maastrichtian successions using carbon-isotope stratigraphy: development of a new Maastrichtian timescale

Cited by 161 publications

References 104 publications

Inoceramid stratigraphy and depositional architecture of the Campanian and Maastrichtian of the Miechów Synclinorium (southern Poland)

Inoceramid stratigraphy and depositional architecture of the Campanian and Maastrichtian of the Miechów Synclinorium (southern Poland)

Transitional environments of the lower Maastrichtian South-Pyrenean Basin (Catalonia, Spain): The Fumanya Member tidal flat

High-resolution Campanian–Maastrichtian carbon and oxygen stable isotopes of bulk-rock and skeletal components: palaeoceanographic and palaeoenvironmental implications for the Boreal shelf sea

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