Global Boundary Stratotype Section and Point for base of Hettangian
E196701
The Global Boundary Stratotype Section and Point for the base of the Hettangian is the internationally agreed geological reference point that marks the formal beginning of the Jurassic Period and the Mesozoic era’s post-Triassic recovery interval.
All labels observed (3)
| Label | Occurrences |
|---|---|
| GSSP for base of Hettangian | 1 |
| Global Boundary Stratotype Section and Point for base of Hettangian canonical | 1 |
| Triassic–Jurassic boundary GSSP | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T1758891 — 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: Global Boundary Stratotype Section and Point for base of Hettangian Context triple: [Early Jurassic, stratotypeDefinedBy, Global Boundary Stratotype Section and Point for base of Hettangian]
-
A.
Global Boundary Stratotype Section and Point at Klonk, Czech Republic
The Global Boundary Stratotype Section and Point at Klonk in the Czech Republic is a formally designated geological reference site that marks the internationally agreed base of the Devonian System and serves as a key standard for correlating Early Devonian rock strata worldwide.
-
B.
International Chronostratigraphic Chart
The International Chronostratigraphic Chart is the globally recognized standard timeline used by geologists to define and correlate the divisions of Earth’s geological history.
-
C.
Siccar Point unconformity
The Siccar Point unconformity is a famous geological site in Scotland where dramatically tilted older rocks are overlain by younger strata, providing key evidence for deep geological time and helping to establish modern geology.
-
D.
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.
-
E.
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.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Global Boundary Stratotype Section and Point for base of Hettangian Target entity description: The Global Boundary Stratotype Section and Point for the base of the Hettangian is the internationally agreed geological reference point that marks the formal beginning of the Jurassic Period and the Mesozoic era’s post-Triassic recovery interval.
-
A.
Global Boundary Stratotype Section and Point at Klonk, Czech Republic
The Global Boundary Stratotype Section and Point at Klonk in the Czech Republic is a formally designated geological reference site that marks the internationally agreed base of the Devonian System and serves as a key standard for correlating Early Devonian rock strata worldwide.
-
B.
International Chronostratigraphic Chart
The International Chronostratigraphic Chart is the globally recognized standard timeline used by geologists to define and correlate the divisions of Earth’s geological history.
-
C.
Siccar Point unconformity
The Siccar Point unconformity is a famous geological site in Scotland where dramatically tilted older rocks are overlain by younger strata, providing key evidence for deep geological time and helping to establish modern geology.
-
D.
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.
-
E.
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.
- F. None of above. chosen
Statements (37)
| Predicate | Object |
|---|---|
| instanceOf |
Global Boundary Stratotype Section and Point
ⓘ
chronostratigraphic reference point ⓘ geological boundary stratotype ⓘ |
| appliesTo | Mesozoic Era ⓘ |
| approvedBy | International Union of Geological Sciences ⓘ |
| belongsToDiscipline |
geology
ⓘ
stratigraphy ⓘ |
| definedBy | International Commission on Stratigraphy ⓘ |
| definesBoundaryBetween |
Jurassic Period
ⓘ
surface form:
Jurassic System
Triassic ⓘ
surface form:
Triassic System
|
| definesBoundaryType | chronostratigraphic boundary ⓘ |
| follows |
Late Triassic
ⓘ
Rhaetian Stage ⓘ |
| hasAbbreviation |
Global Boundary Stratotype Section and Point for base of Hettangian
self-linksurface differs
ⓘ
surface form:
GSSP for base of Hettangian
|
| hasGlobalStatus | ratified international standard ⓘ |
| hasRank | stage boundary ⓘ |
| hasStratigraphicLevel |
series boundary
ⓘ
stage boundary ⓘ system boundary ⓘ |
| hasTemporalContext | post-mass-extinction recovery after end-Triassic extinction ⓘ |
| hasTemporalPosition | earliest Jurassic ⓘ |
| isGlobalStandardFor |
Triassic–Jurassic extinction event
ⓘ
surface form:
Triassic–Jurassic boundary
base of Hettangian Stage ⓘ base of Jurassic System ⓘ |
| isPartOf |
International Chronostratigraphic Chart
ⓘ
surface form:
International Stratigraphic Chart
|
| isReferenceFor |
chemostratigraphic studies of Triassic–Jurassic transition
ⓘ
paleontological zonation across Triassic–Jurassic boundary ⓘ sedimentological studies of Triassic–Jurassic transition ⓘ |
| marksBaseOf |
Hettangian stage
ⓘ
surface form:
Hettangian Stage
Jurassic Period ⓘ Jurassic Period ⓘ
surface form:
Jurassic System
Early Jurassic ⓘ
surface form:
Lower Jurassic Series
post-Triassic recovery interval of the Mesozoic Era ⓘ |
| precedes |
Pliensbachian
ⓘ
surface form:
Sinemurian Stage
|
| usedFor |
geological time scale calibration
ⓘ
global chronostratigraphic correlation ⓘ intercontinental stratigraphic correlation ⓘ |
How these facts were elicited
The pipeline generated the facts above by prompting gpt-5.1 with this entity's name + description and the instruction below.
You are a knowledge base construction expert. Given a subject entity and a description of it, return factual statements that you know for the subject as a JSON list of dictionaries(triples), where keys must be "subject", "predicate" and "object". The number of facts may be very high, between 25 to 50 or more, for very popular subjects. For less popular subjects, the number of facts can be very low, like 5 or 10. # Requirements - If you don't know the subject at all, return an empty list. - If the subject is not a named entity, return an empty list. - Include at least one triple where predicate is "instanceOf". - Do not get too wordy. - Separate several objects into multiple triples with one object.
Subject: Global Boundary Stratotype Section and Point for base of Hettangian Description of subject: The Global Boundary Stratotype Section and Point for the base of the Hettangian is the internationally agreed geological reference point that marks the formal beginning of the Jurassic Period and the Mesozoic era’s post-Triassic recovery interval.
Referenced by (3)
Full triples — surface form annotated when it differs from this entity's canonical label.