Mesoproterozoic Era

E45387

The Mesoproterozoic Era was a middle division of Earth's Proterozoic Eon characterized by the stabilization of continental cratons, widespread sedimentary basin development, and significant evolutionary advances in eukaryotic life.

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All labels observed (2)

Label Occurrences
Mesoproterozoic Era canonical 11
Middle Proterozoic 1

Statements (46)

Predicate Object
instanceOf geologic era
subdivision of the Proterozoic Eon
associatedWith Grenville orogeny
continental collision events
growth of continental crust
atmosphericCondition oxygen levels lower than modern atmosphere
relatively stable oxygen levels compared to Paleoproterozoic
biologicalSignificance appearance of complex multicellular eukaryotes
development of more complex protistan ecosystems
diversification of eukaryotes
expansion of photosynthetic eukaryotic algae
characterizedBy assembly of the supercontinent Rodinia
evolutionary advances in eukaryotic life
extensive platform cover sediments
large passive continental margins
rifting and breakup of earlier supercratons
stabilization of continental cratons
widespread sedimentary basin development
chronostratigraphicUnit Erathem
climate absence of global-scale Snowball Earth glaciations
generally warm climate
contains Calymmian Period
Ectasian Period
Stenian Period
definedBy absolute age boundaries at 1600 Ma and 1000 Ma
duration approximately 600 million years
economicSignificance deposition of important sediment-hosted mineral deposits
formation of some large iron and base metal deposits
end 1000 million years ago
followedBy Neoproterozoic Era
follows Paleoproterozoic Era
geochronologicRank era
notableEvent early stages of Rodinia supercontinent assembly
onset and development of the Grenville orogenic cycle
stabilization of many shield areas
paleogeography development of large shallow epicontinental seas
dominance of stable cratonic blocks
partOf Proterozoic Eon
positionInPrecambrian middle era of the Proterozoic Eon
part of the Precambrian Supereon
precededBy Great Oxidation Event
sedimentaryRecord abundant stromatolitic carbonates
extensive siliciclastic successions
large, long-lived basins
start 1600 million years ago
timeScaleStandard International Commission on Stratigraphy

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.

Instruction
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.
Input
Subject: Mesoproterozoic Era
Description of subject: The Mesoproterozoic Era was a middle division of Earth's Proterozoic Eon characterized by the stabilization of continental cratons, widespread sedimentary basin development, and significant evolutionary advances in eukaryotic life.

Referenced by (12)

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

Proterozoic Eon subdivision Mesoproterozoic Era
Precambrian Supereon contains Mesoproterozoic Era
Paleoproterozoic Era precedes Mesoproterozoic Era
Neoproterozoic Era follows Mesoproterozoic Era
Grenville orogeny geologicEra Mesoproterozoic Era
Calymmian Period partOf Mesoproterozoic Era
Calymmian Period geologicEra Mesoproterozoic Era
Ectasian Period partOf Mesoproterozoic Era
Ectasian Period fallsWithin Mesoproterozoic Era
this entity surface form: Middle Proterozoic
Ectasian Period era Mesoproterozoic Era
Stenian Period partOf Mesoproterozoic Era
Stenian Period geologicEra Mesoproterozoic Era