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.

All labels observed (1)

Label Occurrences
Hangenberg black shales canonical 1

How this entity was disambiguated

Statements (44)

Predicate Object
instanceOf black shale ⓘ
sedimentary rock unit ⓘ
stratigraphic unit ⓘ
associatedEvent Hangenberg crisis ⓘ
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 ⓘ
linked to: Famennian stage

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 ⓘ

How these facts were elicited

Referenced by (1)

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

Late Devonian extinction → hasStratigraphicMarker → Hangenberg black shales ⓘ