Hangenberg black shales

E415308

The Hangenberg black shales are organic-rich Late Devonian sedimentary deposits that record the environmental and oceanographic upheavals associated with the Hangenberg extinction event.

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All labels observed (1)

Label Occurrences
Hangenberg black shales canonical 1

Statements (44)

Predicate Object
instanceOf black shale
sedimentary rock unit
stratigraphic unit
associatedEvent Frasnian–Famennian boundary
surface form: Hangenberg crisis

Late Devonian extinction
surface form: Hangenberg extinction event
chronostratigraphicRole marker horizon for the Hangenberg event
used for interbasinal correlation of the Devonian–Carboniferous boundary
color black
depositionalEnvironment basinal
dysoxic to anoxic seafloor conditions
marine
economicSignificance potential source rock for hydrocarbons in some basins
formationProcess deposited during intervals of reduced bottom-water oxygenation
formed under conditions of enhanced preservation of organic matter
fossilContent contains conodonts
contains microfossils indicative of stressed marine ecosystems
contains palynomorphs
geochemicalCharacteristic enriched in redox-sensitive trace metals
high total organic carbon content
often show positive excursions in organic carbon isotopes
geographicDistribution recorded in multiple Late Devonian basins worldwide
reported from North African basins
reported from North American basins
well documented in European sections
geologicAge Famennian stage
surface form: Famennian

Late Devonian
lithology fine-grained siliciclastic sedimentary rock
organic-rich shale
oxygenationIndicator lack of bioturbation indicates low-oxygen bottom waters
paleoenvironmentalSignificance evidence for global carbon cycle perturbations
evidence for widespread marine anoxia
record environmental upheavals at the end of the Devonian
record oceanographic changes associated with the Hangenberg extinction event
relatedTo Hangenberg Sandstone
Hangenberg event beds
researchUse used to investigate global sea-level changes at the Devonian–Carboniferous transition
used to reconstruct paleo-redox conditions
used to study Late Devonian mass extinction dynamics
sedimentaryStructure typically laminated
stratigraphicContext part of the Hangenberg Event succession in many sections
stratigraphicPosition overlain by early Carboniferous strata
uppermost Devonian
temporalRelation associated with the Devonian–Carboniferous boundary
followed the Kellwasser events of the Late Devonian

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Late Devonian extinction hasStratigraphicMarker Hangenberg black shales