Rodinia

GPTKB entity

Properties (60)
Predicate Object
gptkbp:instanceOf supercontinent
gptkbp:associated_with the assembly of continents
the breakup of ancient landmasses
the breakup of the supercontinent cycle
the development of rift valleys
the evolution of land plants
the evolution of plate tectonics
the_Proterozoic_Eon
gptkbp:composedOf most_of_Earth's_landmasses
gptkbp:contains cratons
gptkbp:contributedTo mass extinction events
gptkbp:disassembly 750 million years ago
gptkbp:formed 1.3 billion years ago
continental_collision
gptkbp:has_a_focus_on geological modeling
geological conferences
paleobiology research
gptkbp:has_a_role_in the development of ecosystems
gptkbp:has_implications_for ocean circulation patterns
gptkbp:hasConflictWith glaciation events
gptkbp:hasRecognition the Neoproterozoic Era
https://www.w3.org/2000/01/rdf-schema#label Rodinia
gptkbp:is_a_key_component_of the_study_of_Earth's_history
gptkbp:is_a_subject_of academic research
geological research
paleogeography
paleomagnetic studies
geological modeling studies
gptkbp:is_characterized_by extensive volcanic activity
large continental masses
gptkbp:is_essential_for understanding continental drift
understanding continental formation
understanding_Earth's_geological_history
understanding_Earth's_past_climates
understanding_Earth's_tectonic_history
gptkbp:is_expected_to a precursor to modern continents
gptkbp:is_featured_in geological maps
gptkbp:is_linked_to the study of ancient climates
the formation of mountain ranges
the evolution of early life
the formation of sedimentary basins
gptkbp:is_located_in southern hemisphere
gptkbp:is_part_of Earth's_geological_timeline
gptkbp:is_studied_in plate tectonics
tectonic activity
geological surveys
gptkbp:is_used_in scientific literature
geological textbooks
geological evidence
other supercontinents
scientific discussions about supercontinents
gptkbp:precededBy the_supercontinent_Nuna
gptkbp:related_to climate change studies
the study of mineral deposits
gptkbp:religion global climate
biological evolution
the distribution of fossils
the distribution of minerals
gptkbp:succeededBy the_supercontinent_Pannotia
gptkbp:was_marked_by geologist_Joseph_Meert