The Jurassic–Cretaceous boundary interval in non-marine strata of northwest Europe: New light on an old problem

Research output: Contribution to journalArticleResearchpeer review

Authors

External Research Organisations

  • Ruhr-Universität Bochum
  • State Authority for Mining, Energy and Geology (LBEG)
View graph of relations

Details

Original languageEnglish
Pages (from-to)42-54
Number of pages13
JournalCretaceous Research
Volume87
Early online date16 Jun 2017
Publication statusPublished - Jul 2018

Abstract

The non-marine Purbeck- and Wealden-type sediments of latest Jurassic (Tithonian) and earliest Cretaceous (Berriasian) age in northern Germany were deposited in a restricted intercontinental basin. They mark an interval of strong faunal and floral provincialism which makes correlation of the non-marine strata across northwest Europe difficult. The position of the Jurassic–Cretaceous boundary has therefore been debated for decades. Our integrated stratigraphy of four sections in northern Germany, based on palynology (spores, pollen, dinoflagellate cysts) and ostracods, provides new evidence for a precise correlation with contemporaneous strata of other non-marine basins in northwest Europe. Correlation with the marine Boreal Realm and the Tethys is achieved via the Purbeck type section in England. A stratigraphic subdivision of the non-marine Berriasian succession in Germany is possible by using seven short-lived marine flooding events, which are documented by ceratioid dinoflagellate cysts and foraminifera. Our data suggest that a first major transgression took place close to the base of the Boreal Surites stenomphalus ammonite Zone. This level corresponds to a contemporaneous flooding event in southern England (Scallop Beds, Purbeck Group) and in southern Sweden (Annero Formation), thereby providing an excellent marker horizon for interbasinal correlation.

Keywords

    Correlations, Dinoflagellates, Lower Cretaceous, Ostracods, Palynology

ASJC Scopus subject areas

Sustainable Development Goals

Cite this

The Jurassic–Cretaceous boundary interval in non-marine strata of northwest Europe: New light on an old problem. / Schneider, Anton Christoph; Heimhofer, Ulrich; Heunisch, Carmen et al.
In: Cretaceous Research, Vol. 87, 07.2018, p. 42-54.

Research output: Contribution to journalArticleResearchpeer review

Schneider AC, Heimhofer U, Heunisch C, Mutterlose J. The Jurassic–Cretaceous boundary interval in non-marine strata of northwest Europe: New light on an old problem. Cretaceous Research. 2018 Jul;87:42-54. Epub 2017 Jun 16. doi: 10.1016/j.cretres.2017.06.002
Download
@article{440e82265d7940fb9fc281654580e6c3,
title = "The Jurassic–Cretaceous boundary interval in non-marine strata of northwest Europe: New light on an old problem",
abstract = "The non-marine Purbeck- and Wealden-type sediments of latest Jurassic (Tithonian) and earliest Cretaceous (Berriasian) age in northern Germany were deposited in a restricted intercontinental basin. They mark an interval of strong faunal and floral provincialism which makes correlation of the non-marine strata across northwest Europe difficult. The position of the Jurassic–Cretaceous boundary has therefore been debated for decades. Our integrated stratigraphy of four sections in northern Germany, based on palynology (spores, pollen, dinoflagellate cysts) and ostracods, provides new evidence for a precise correlation with contemporaneous strata of other non-marine basins in northwest Europe. Correlation with the marine Boreal Realm and the Tethys is achieved via the Purbeck type section in England. A stratigraphic subdivision of the non-marine Berriasian succession in Germany is possible by using seven short-lived marine flooding events, which are documented by ceratioid dinoflagellate cysts and foraminifera. Our data suggest that a first major transgression took place close to the base of the Boreal Surites stenomphalus ammonite Zone. This level corresponds to a contemporaneous flooding event in southern England (Scallop Beds, Purbeck Group) and in southern Sweden (Annero Formation), thereby providing an excellent marker horizon for interbasinal correlation.",
keywords = "Correlations, Dinoflagellates, Lower Cretaceous, Ostracods, Palynology",
author = "Schneider, {Anton Christoph} and Ulrich Heimhofer and Carmen Heunisch and J{\"o}rg Mutterlose",
note = "Publisher Copyright: {\textcopyright} 2017 Elsevier Ltd Copyright: Copyright 2018 Elsevier B.V., All rights reserved.",
year = "2018",
month = jul,
doi = "10.1016/j.cretres.2017.06.002",
language = "English",
volume = "87",
pages = "42--54",
journal = "Cretaceous Research",
issn = "0195-6671",
publisher = "Academic Press Inc.",

}

Download

TY - JOUR

T1 - The Jurassic–Cretaceous boundary interval in non-marine strata of northwest Europe

T2 - New light on an old problem

AU - Schneider, Anton Christoph

AU - Heimhofer, Ulrich

AU - Heunisch, Carmen

AU - Mutterlose, Jörg

N1 - Publisher Copyright: © 2017 Elsevier Ltd Copyright: Copyright 2018 Elsevier B.V., All rights reserved.

PY - 2018/7

Y1 - 2018/7

N2 - The non-marine Purbeck- and Wealden-type sediments of latest Jurassic (Tithonian) and earliest Cretaceous (Berriasian) age in northern Germany were deposited in a restricted intercontinental basin. They mark an interval of strong faunal and floral provincialism which makes correlation of the non-marine strata across northwest Europe difficult. The position of the Jurassic–Cretaceous boundary has therefore been debated for decades. Our integrated stratigraphy of four sections in northern Germany, based on palynology (spores, pollen, dinoflagellate cysts) and ostracods, provides new evidence for a precise correlation with contemporaneous strata of other non-marine basins in northwest Europe. Correlation with the marine Boreal Realm and the Tethys is achieved via the Purbeck type section in England. A stratigraphic subdivision of the non-marine Berriasian succession in Germany is possible by using seven short-lived marine flooding events, which are documented by ceratioid dinoflagellate cysts and foraminifera. Our data suggest that a first major transgression took place close to the base of the Boreal Surites stenomphalus ammonite Zone. This level corresponds to a contemporaneous flooding event in southern England (Scallop Beds, Purbeck Group) and in southern Sweden (Annero Formation), thereby providing an excellent marker horizon for interbasinal correlation.

AB - The non-marine Purbeck- and Wealden-type sediments of latest Jurassic (Tithonian) and earliest Cretaceous (Berriasian) age in northern Germany were deposited in a restricted intercontinental basin. They mark an interval of strong faunal and floral provincialism which makes correlation of the non-marine strata across northwest Europe difficult. The position of the Jurassic–Cretaceous boundary has therefore been debated for decades. Our integrated stratigraphy of four sections in northern Germany, based on palynology (spores, pollen, dinoflagellate cysts) and ostracods, provides new evidence for a precise correlation with contemporaneous strata of other non-marine basins in northwest Europe. Correlation with the marine Boreal Realm and the Tethys is achieved via the Purbeck type section in England. A stratigraphic subdivision of the non-marine Berriasian succession in Germany is possible by using seven short-lived marine flooding events, which are documented by ceratioid dinoflagellate cysts and foraminifera. Our data suggest that a first major transgression took place close to the base of the Boreal Surites stenomphalus ammonite Zone. This level corresponds to a contemporaneous flooding event in southern England (Scallop Beds, Purbeck Group) and in southern Sweden (Annero Formation), thereby providing an excellent marker horizon for interbasinal correlation.

KW - Correlations

KW - Dinoflagellates

KW - Lower Cretaceous

KW - Ostracods

KW - Palynology

UR - http://www.scopus.com/inward/record.url?scp=85020686758&partnerID=8YFLogxK

U2 - 10.1016/j.cretres.2017.06.002

DO - 10.1016/j.cretres.2017.06.002

M3 - Article

AN - SCOPUS:85020686758

VL - 87

SP - 42

EP - 54

JO - Cretaceous Research

JF - Cretaceous Research

SN - 0195-6671

ER -

By the same author(s)