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
This entity first appeared as the object of triple T4145623 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
Target entity: Hangenberg black shales Context triple: [Late Devonian extinction, hasStratigraphicMarker, Hangenberg black shales]
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A.
Solnhofen Limestone
Solnhofen Limestone is a famous Late Jurassic lithographic limestone formation in Bavaria, Germany, renowned for its exceptionally well-preserved fossils, including the iconic Archaeopteryx.
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B.
Burgess Shale fossil lagerstätte
The Burgess Shale fossil lagerstätte is a renowned Middle Cambrian rock formation in the Canadian Rockies famous for its exceptionally well-preserved soft-bodied fossils that reveal the diversity of early animal life.
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C.
Rhynie Chert fossil locality
The Rhynie Chert fossil locality is a famous Early Devonian site in Scotland renowned for its exceptionally preserved early land plants, arthropods, and microorganisms that provide key insights into the evolution of terrestrial ecosystems.
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D.
Hettange-Grande Formation
The Hettange-Grande Formation is an Early Jurassic (Hettangian) sedimentary rock unit in northeastern France that serves as the global stratotype (type section) for the base of the Jurassic System.
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E.
Claron Formation
The Claron Formation is a geologic rock unit of colorful limestones and mudstones best known for forming the striking hoodoos and cliffs of Bryce Canyon and other parts of the Paunsaugunt Plateau in southern Utah.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Hangenberg black shales Target entity description: The Hangenberg black shales are organic-rich Late Devonian sedimentary deposits that record the environmental and oceanographic upheavals associated with the Hangenberg extinction event.
-
A.
Solnhofen Limestone
Solnhofen Limestone is a famous Late Jurassic lithographic limestone formation in Bavaria, Germany, renowned for its exceptionally well-preserved fossils, including the iconic Archaeopteryx.
-
B.
Burgess Shale fossil lagerstätte
The Burgess Shale fossil lagerstätte is a renowned Middle Cambrian rock formation in the Canadian Rockies famous for its exceptionally well-preserved soft-bodied fossils that reveal the diversity of early animal life.
-
C.
Rhynie Chert fossil locality
The Rhynie Chert fossil locality is a famous Early Devonian site in Scotland renowned for its exceptionally preserved early land plants, arthropods, and microorganisms that provide key insights into the evolution of terrestrial ecosystems.
-
D.
Hettange-Grande Formation
The Hettange-Grande Formation is an Early Jurassic (Hettangian) sedimentary rock unit in northeastern France that serves as the global stratotype (type section) for the base of the Jurassic System.
-
E.
Claron Formation
The Claron Formation is a geologic rock unit of colorful limestones and mudstones best known for forming the striking hoodoos and cliffs of Bryce Canyon and other parts of the Paunsaugunt Plateau in southern Utah.
- F. None of above. chosen
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 ⓘ |
How these facts were elicited
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Subject: Hangenberg black shales Description of subject: The Hangenberg black shales are organic-rich Late Devonian sedimentary deposits that record the environmental and oceanographic upheavals associated with the Hangenberg extinction event.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.