Kellwasser horizons

E415307

The Kellwasser horizons are distinctive black shale layers in Late Devonian marine sediments that mark one of the major extinction pulses during the Late Devonian mass extinction.

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All labels observed (2)

Label Occurrences
Kellwasser horizons canonical 2
Lower Kellwasser event 1

Statements (39)

Predicate Object
instanceOf black shale unit
event bed
geological horizon
stratigraphic marker
age Frasnian–Famennian boundary interval
associatedWith Late Devonian extinction
surface form: Frasnian–Famennian extinction event

Late Devonian extinction
surface form: Late Devonian mass extinction

crisis in stromatoporoids and corals
decline of reef-building organisms
extinction of many marine invertebrate taxa
contains laminated black shale
organic-rich mudstone
pyrite
correlatesWith global sea-level changes in the Late Devonian
widespread marine anoxia events
discoveredIn 19th century
environment marine
geochemicalSignature enrichment in redox-sensitive trace metals
high total organic carbon
negative carbon isotope excursions
geologicalPeriod Late Devonian
lithology black shale
marks extinction pulse during the Late Devonian mass extinction
namedAfter Kellwassertal in the Harz Mountains, Germany
occursIn Europe
North America
global marine basins
paleoenvironmentalInterpretation anoxic bottom-water conditions
eutrophication of marine basins
researchTopicIn Devonian stratigraphy
mass extinction studies
paleoceanography
significance key marker for the Late Devonian biotic crisis
stratigraphicPosition uppermost Frasnian
subdivision Lower Kellwasser horizon
Upper Kellwasser horizon
temporalRelation immediately precede the Frasnian–Famennian boundary
usedAs biostratigraphic marker
chemostratigraphic marker

Referenced by (3)

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

Kellwasser events hasPart Kellwasser horizons
this entity surface form: Lower Kellwasser event
Kellwasser events recordedIn Kellwasser horizons