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Hypothesized Neoproterozoic supercontinent
Pannotia (from Greek: pan-, "all", -nótos, "south"; meaning "all southern land"), also known as the Vendian supercontinent, Greater Gondwana, and the Pan-African
Pannotia
Northern landmass that formed part of the Pangaea supercontinent
each other within the short-lived, Precambrian-Cambrian supercontinent Pannotia or Greater Gondwana. At this time a series of continental blocks called
Laurasia
Craton forming the geological core of North America
fragments of Rodinia gathered into another short-lived supercontinent, Pannotia, at the very end of the Proterozoic. This continent broke up again almost
Laurentia
Ocean that surrounds a supercontinent
Rodinia, and Panthalassa, which surrounded the supercontinent Pangaea. Pannotia and Columbia, along with landmasses before Columbia (such as Ur and Kenorland)
Superocean
Hypothetical Neoproterozoic supercontinent
with its continental fragments reassembled to form Pannotia 633–573 Ma. In contrast with Pannotia, little is known about Rodinia's configuration and geodynamic
Rodinia
First era of the Phanerozoic Eon
breakup of the supercontinent of Pannotia and ended while the supercontinent Pangaea was assembling. The breakup of Pannotia began with the opening of the
Paleozoic
Supercontinent from the late Paleozoic to early Mesozoic eras
are not nearly as well understood as those of the later supercontinents, Pannotia and Pangaea. According to one reconstruction, when Rodinia broke up, it
Pangaea
First geological period of the Paleozoic Era
ongoing debate around the existence of the Neoproterozoic supercontinent of Pannotia, means that while most models agree the continents lay in the southern
Cambrian
Records of Earth's development
around 550 Ma. The hypothetical supercontinent is sometimes referred to as Pannotia or Vendia. The evidence for it is a phase of continental collision known
History_of_Earth
Rodinia, began to break apart. The continents later recombined to form Pannotia, 600 to 540 million years ago, then finally Pangaea, which broke apart
Geological_history_of_Earth
Mostly submerged continental crust area in Oceania
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
Zealandia
Third planet from the Sun
Rodinia, began to break apart. The continents later recombined to form Pannotia at 600–540 Ma, then finally Pangaea, which also began to break apart at
Earth
Retrieved 28 November 2015. Scotese 2009, Reconstruction of Rodinia and Pannotia, p. 68 Bradley, D.C. (2011). "Secular Trends in the Geologic Record and
Chronology_of_continents
Largest ocean
ISBN 978-0-387-98313-4. "GEOL 102 The Proterozoic Eon II: Rodinia and Pannotia". Geol.umd.edu. 5 January 2010. Retrieved 31 October 2010. Mussett, Alan
Pacific_Ocean
Majority of lands of the Western Hemisphere
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
New_World
Large geographical region identified by convention
continental cores. These have included Vaalbara, Kenorland, Columbia, Rodinia, Pannotia, and Pangaea. Over time, these supercontinents broke apart into large landmasses
Continent
Second period of the Neoproterozoic Era, with major glaciation
cratons (possibly) later assembled into another supercontinent called Pannotia, in the Ediacaran. Eyles and Young state, "Most Neoproterozoic glacial
Cryogenian
Failed microcontinent between Greenland and Canada
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
Davis Strait proto-microcontinent
Davis_Strait_proto-microcontinent
Landmass corresponding to Afro–Eurasia
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
Old_World
Fictional island in Plato's works
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
Atlantis
Landmass comprising more than one continental core, or craton
(Nuna) 1,820–1,350 Orosirian-Ectasian Rodinia 1,130–750 Stenian-Tonian Pannotia 633–573 Ediacaran Gondwana 550–175 Ediacaran-Jurassic From the Carboniferous
Supercontinent
Repeated joining and separation of Earth's continents
to 2.1 Ga); Columbia (1.8 to 1.5 Ga); Rodinia (1.25 Ga to 750 Ma); and Pannotia (c. 600 Ma), whose dispersal produced the continents that ultimately collided
Supercontinent_cycle
006. Nance, R.D.; Murphy, J.B. (2019). "Supercontinents and the case for Pannotia". In Wilson, R.W.; Houseman, G.A.; McCaffrey, K.J.W.; Doré, A.G.; Buiter
List_of_paleocontinents
Scientific study of Earth's physical composition
ago): Rodinia supercontinent 730–635 Ma: second snowball Earth 650–540 Ma: Pannotia supercontinent 541±0.3 Ma: Cambrian explosion – vast multiplication of
Geology
Geologic eon, 2500–539 million years ago
magnitude after every period. Columbia, about 1,590 Ma Rodinia, about 900 Ma Pannotia, 545 Ma (disputed[clarification needed]), centered on South Pole Gondwana
Proterozoic
between plates separating supercontinent fragments Gondwana and Pannotia – Supercontinent Pannotia (to c. 500 Ma) completed, bordered by Iapetus and Panthalassa
Timeline_of_Earth
Ancient craton forming the Central Siberian Plateau
Protolaurasia became part of the southern supercontinent of Pannotia. Around 550 million years ago, both Pannotia and Protolaurasia split up to become the continents
Siberia_(continent)
Neoproterozoic to Cretaceous landmass
Cambrian boundary, forming the short-lived and still disputed supercontinent Pannotia. The Mozambique Ocean separated the Congo–Tanzania–Bangweulu Block of central
Gondwana
Material world and its phenomena
Rodinia, began to break apart. The continents later recombined to form Pannotia which broke apart about 540 million years ago, then finally Pangaea, which
Nature
Local variation of the Earth's magnetic field in central Africa
Parts of South America and Africa around 545 Ma. See also Pannotia.
Bangui_magnetic_anomaly
Small Precambrian ocean between Baltica and the Siberian continent
formed when the landmass of Proto-Laurasia (shortly after the break-up of Pannotia, about 600 mya) rifted and created three separated continents – Laurentia
Khanty_Ocean
Hypothetical Archaean supercontinent from about 3.6 to 2.7 billion years ago
orogeny. The Neoproterozoic Pan-African orogeny and the assembly of Gondwana/Pannotia produced large shear zones between Grunehogna and Kalahari. During the
Vaalbara
Cratonic rock body which makes up most of the continent Antarctica
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
East_Antarctic_Shield
Third and last period of the Neoproterozoic Era
record in the last few million years of the Ediacaran. The supercontinent Pannotia formed and broke apart by the end of the period. The Ediacaran also witnessed
Ediacaran
Series of major mountain-forming events in the Neoproterozoic
events which related to the formation of the supercontinents Gondwana and Pannotia about 600 million years ago. This orogeny is also known as the Pan-Gondwanan
Pan-African_orogeny
Hypothetical continent
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
Terra_Australis
Geology of U.S. state
the current west coast of South America in the west of the short-lived Pannotia supercontinent. Africa, South America, Australia, India and Antarctica
Geology_of_Massachusetts
Last period of the Mesoproterozoic Era
tectonics and palaeogeography: a tale of two supercontinents, Rodinia and Pannotia". Geological Society of London, Special Publications. 326 (1): 67–83. Bibcode:2009GSLSP
Stenian
Large area of continental crust in the north-central part of Africa
Pannotia super-continent c. 570 Ma
Saharan_Metacraton
Topics referred to by the same term
Australian islands. Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Arctica Asiamerica Atlantica Avalonia Baltica Cimmeria
Forgotten_continent
Fourth and current eon of the geological timescale
animals evolved in this period. During this time, the super-continent Pannotia began to break up, most of which later recombined into the super-continent
Phanerozoic
Hypothesized paleo-ocean whose closure created the supercontinent of Pannotia
a hypothesized paleo-ocean whose closure created the supercontinent of Pannotia. The ocean may have existed before the break-up of the supercontinent of
Pan-African_Ocean
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
List_of_Indigenous_peoples
Exposure of Precambrian crystalline rocks on the flanks of the Red Sea
The Arabian-Nubian Shield in the supercontinent Pannotia c. 570 million years ago, before the opening of the Red Sea.
Arabian-Nubian_Shield
Geological feature
ancient, active southern margin of the supercontinents Rodinia and later Pannotia (also called Greater Gondwana). This vast orogenic belt stretched for approximately
Terra_Australis_Orogen
Mountains in the US state Oklahoma
region began to rift apart during breakup of the Neoproterozoic continent, Pannotia. The exposed portion of this unit, named the Glen Mountains Layered Complex
Wichita_Mountains
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
List of sovereign states and dependent territories by continent
List_of_sovereign_states_and_dependent_territories_by_continent
List of Earth's former oceans
and the Hunic terranes Pan-African Ocean, the ocean that surrounded the Pannotia supercontinent Panthalassa, the vast world ocean that surrounded the Pangaea
List_of_ancient_oceans
Prehistoric supercontinents Columbia Gondwana Kenorland Laurasia Nena Pangaea Pannotia Rodinia Ur Vaalbara Other prehistoric continents Amazonia Appalachia Arctica
List of sovereign states and dependent territories by continent (data file)
List_of_sovereign_states_and_dependent_territories_by_continent_(data_file)
Ancient microcontinent now part of Argentina
virtually all continents formed a "proto-Gondwana" supercontinent known as Pannotia. The Precordillera was then part of a proposed "Texas Plateau", a promontory
Cuyania
Main stage in the Neoproterozoic assembly of East and West Gondwana
Gondwana: polyphase or simple?, pp. 9–11; Nance, Murphy & Santosh 2014, Pannotia (Gondwana), pp. 12, 14 Azania was defined by Collins & Windley 2002, Discussion
East_African_Orogeny
Protected area in Newfoundland, Canada
that is found in Western Europe. It formed in the early Cambrian when Pannotia broke from Gondwana (now South America, Africa, Antarctica, and Australia)
Mistaken Point Ecological Reserve
Mistaken_Point_Ecological_Reserve
Geological events that formed the Ural Mountains
deformed in the Timanide and Cadomide orogenies or the assembly of the Pannotia supercontinent. The break-up of this supercontinent opened the Palaeo-Uralian
Uralian_orogeny
Earth's dry surface
Rodinia, began to break apart. The continents later recombined to form Pannotia, 600–540 mya, then finally Pangaea, which also broke apart 180 mya. A continuous
Land
part of the Arabian plate that was located on the margin of Rodinia and Pannotia in the Neoproterozoic, and of Gondwana in the Paleozoic and Mesozoic. The
Geology_of_Iran
Hierarchical outline list of articles related to plate tectonics
Pangaea – Supercontinent from the late Paleozoic to early Mesozoic eras Pannotia – Hypothesized Neoproterozoic supercontinent Rodinia – Hypothetical Neoproterozoic
Outline_of_plate_tectonics
Newfoundland) formed as a volcanic island arc off the coast of the supercontinents Pannotia which lost land through rifting and became Gondwana. This volcanic island
Geology of Newfoundland and Labrador
Geology_of_Newfoundland_and_Labrador
Failed arm of a triple junction, an inactive rift zone
formed as a product of intracontinental rifting during the breakup of Pannotia. The Southern Oklahoma Aulacogen is located in southwestern Oklahoma and
Aulacogen
outcroppings of granite bedrock. Starting in the Paleozoic Era the supercontinent Pannotia began to break up, forming smaller continents including Laurentia (North
Geology_of_New_England
established to be just south of the equator as part of the supercontinent Pannotia, contrasting with its present position at 82 degrees southern latitude
Shackleton_Limestone
Ancient ocean that existed from the latest Ediacaran to the Carboniferous
geologists dispute the existence of such an ocean. The ocean formed when Pannotia disintegrated, Proto-Laurasia (Laurentia, Baltica, and Siberia) rifted
Proto-Tethys_Ocean
Cathaysian and Cimmerian Terranes. The name Pangaea is Greek for “all lands”. Pannotia A supercontinent that existed in the Late Precambrian and gave rise to
Glossary_of_history
Accumulated material on seafloor
apart about 700 million years ago. The continents later recombined to form Pannotia, 600 to 540 million years ago, then finally Pangaea, which broke apart
Marine_sediment
One of the five Precambrian cratons that make up the African Plate
West African Craton may then have combined with other cratons to form Pannotia, a hypothetical supercontinent that existed from the Pan-African orogeny
West_African_Craton
former microcontinent of Avalonia. With the breakup of the supercontinent Pannotia beginning 600 million years ago, the new continent of Laurentia—Proto-North
Geology_of_Maine
Ancient ocean that existed from 800 to 635 million years ago
break-up of the Rodinia supercontinent and the start of formation of the Pannotia supercontinent. The Pharusian Ocean opened around 800 million years ago
Pharusian_Ocean
modern CAR was situated near the center of the subsequent supercontinent Pannotia, as part of the fully assembled basement rock of the current African continent
Geology of the Central African Republic
Geology_of_the_Central_African_Republic
Geologic fault in north-west Wales
mainland North Wales". In Murphy, B.; Strachan, R.A.; Quesada, C. (eds.). Pannotia to Pangaea: Neoproterozoic and Paleozoic Orogenic Cycles in the Circum-Atlantic
Berw_Fault
Geologic formation in Northeastern Ontario, Canada
the Congo craton to form the supercontinent Pannotia 600 million years ago. In contrast to Rodinia, Pannotia was short-lived. It rifted apart 545 million
Temagami_Greenstone_Belt
resulted from rifting that took place as the Neoproterozoic supercontinent Pannotia was breaking apart. Isotopic analysis of these intrusive units indicate
Roosevelt_Gabbros
moved northward from Gondwana following the breakup of the supercontinent Pannotia. Rhode Island became landlocked during the formation of Pangaea and experienced
Geology_of_Rhode_Island
Limestone formation in Antarctica
Mountains, Yochelson Ridge & Heritage Range Paleogeography of the Cambrian with the supercontinent Pannotia and Antarctica south of the paleo-equator
Minaret_Formation
Crustal fragment in southeastern U.S.
Central Atlantic magmatic province The formation of the supercontinent Pannotia between 750 and 530 million years ago brought the Amazonian and West African
Suwannee_terrane
its geolocation chronology. In the early Cambrian, the supercontinent Pannotia broke up and Avalonia drifted off northwards from Gondwana. This independent
Geology_of_England
PANNOTIA
PANNOTIA
PANNOTIA
PANNOTIA
Girl/Female
German, Hebrew
Jehovah Increases; Female Version of Joseph
Girl/Female
Biblical
An entry or vestibule.
Boy/Male
Hindu, Indian
Soft Hearted
Boy/Male
English Irish Scottish American Celtic
from the craggy hills.
Girl/Female
Hindu
Hands full of gold i.e. prosperity
Boy/Male
Tamil
Sukanta | ஸà¯à®•à®¨à¯à®¤à®¾
Handsome
Girl/Female
Latin Spanish Italian
Blooming.
Boy/Male
Arabic, Hindu, Indian
Handsome
Boy/Male
Irish Anglo Saxon
White.
Girl/Female
Tamil
Safety, Security, Welfare, Tranquility, Goddess Durga
PANNOTIA
PANNOTIA
PANNOTIA
PANNOTIA
PANNOTIA