This HTML5 document contains 159 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
dctermshttp://purl.org/dc/terms/
dbohttp://dbpedia.org/ontology/
n17http://dbpedia.org/resource/File:
foafhttp://xmlns.com/foaf/0.1/
n4https://books.google.com/
n15https://global.dbpedia.org/id/
dbthttp://dbpedia.org/resource/Template:
rdfshttp://www.w3.org/2000/01/rdf-schema#
n14http://commons.wikimedia.org/wiki/Special:FilePath/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
owlhttp://www.w3.org/2002/07/owl#
wikipedia-enhttp://en.wikipedia.org/wiki/
dbphttp://dbpedia.org/property/
provhttp://www.w3.org/ns/prov#
dbchttp://dbpedia.org/resource/Category:
xsdhhttp://www.w3.org/2001/XMLSchema#
wikidatahttp://www.wikidata.org/entity/
dbrhttp://dbpedia.org/resource/

Statements

Subject Item
dbr:Environment_of_New_Zealand
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:Geology_of_New_Zealand
rdfs:seeAlso
dbr:Natural_history_of_New_Zealand
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:Geography_of_New_Zealand
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:Banks_Peninsula_Volcano
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:Foulden_Maar
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:List_of_New_Zealand–related_topics
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:History_of_New_Zealand
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:Natural_history_of_Australia
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:Natural_history_of_New_Zealand
rdf:type
owl:Thing
rdfs:label
Natural history of New Zealand
rdfs:comment
The natural history of New Zealand began when the landmass Zealandia broke away from the supercontinent Gondwana in the Cretaceous period. Before this time, Zealandia shared its past with Australia and Antarctica. Since this separation, the New Zealand landscape has evolved in physical isolation, although much of its current biota has more recent connections with species on other landmasses. The exclusively natural history of the country ended in about 1300 AD, when humans first settled, and the country's environmental history began. The period from 1300 AD to today coincides with the extinction of many of New Zealand's unique species that had evolved there.
rdfs:seeAlso
dbr:South_Polar_region_of_the_Cretaceous
foaf:depiction
n14:Kaiwhekea_NT_small.jpg n14:Zealandia_and_New_Zealand_90_ma_Gondwana.png n14:30_ma_New_Zealand_Zealandia.png n14:Foulden_Maar_reconstruction_by_Paula_Peeters.jpg n14:Bullseye1.png n14:Opening_of_South_Atlantic_83_Ma.png n14:Giant_moa.jpg n14:Nothofagus_demis.jpg
dcterms:subject
dbc:Environment_of_New_Zealand dbc:Geology_of_New_Zealand dbc:Biota_of_New_Zealand dbc:Natural_history_of_New_Zealand
dbo:wikiPageID
15089769
dbo:wikiPageRevisionID
1113355812
dbo:wikiPageWikiLink
dbr:Monotreme dbr:Gondwana dbr:South_America dbr:Laurel_forest dbr:Southern_Alps dbc:Environment_of_New_Zealand dbc:Geology_of_New_Zealand dbr:Coal dbr:Eocene dbr:Podocarpaceae dbr:Last_glacial_maximum dbr:New_Zealand_wren dbr:Northland_Region dbr:Miocene dbr:Queensland dbr:Holocene_extinction dbr:Maar-diatreme_volcano dbr:Taupo_Volcanic_Zone dbr:Angiosperm dbr:Saint_Bathans_Fauna dbr:Murgon_fossil_site dbr:Glaciation dbr:Environment_of_New_Zealand dbr:Antarctic dbr:Utah dbr:Antarctic_Circumpolar_Current dbr:Coprolite dbr:Greenland_ice_sheet dbr:Pleistocene dbr:Maar dbr:Crocodile dbr:Southern_beech dbr:Saurischia dbr:Australian_Plate dbr:Genetic_bottleneck n17:Zealandia_and_New_Zealand_90_ma_Gondwana.png dbr:Ornithischia dbr:Antarctic_flora dbr:Fiordland dbr:Tuatara dbr:Foulden_Maar dbr:Zealandia dbr:Hatepe_eruption n17:Nothofagus_demis.JPG dbr:Antarctic_ice_sheet dbr:Laurissilva dbr:Gondwanatheria dbr:Araucaria dbc:Biota_of_New_Zealand dbr:Tertiary dbr:Cretaceous dbr:Geology_of_New_Zealand dbr:Saint_Bathans_mammal dbr:Laurasia dbr:Biodiversity_of_New_Zealand dbr:Agathis dbr:Lightning_Ridge,_New_South_Wales dbr:Sauropodomorpha n17:Kaiwhekea_NT_small.jpg dbr:Supercontinent dbr:Oligocene dbr:Theria dbr:Nothofagus dbr:New_Zealand_geologic_time_scale dbc:Natural_history_of_New_Zealand n17:Foulden_Maar_reconstruction_by_Paula_Peeters.jpg dbr:Loess dbr:Fossil n17:Opening_of_South_Atlantic_83_Ma.png dbr:Tasman_Sea dbr:Afrotheria dbr:Alpine_Fault dbr:Pacific_Plate dbr:Corynocarpus_laevigatus dbr:List_of_dinosaurs_and_other_Mesozoic_reptiles_of_New_Zealand dbr:Placental n17:30_ma_New_Zealand_Zealandia.png dbr:Cretaceous–Paleogene_extinction_event dbr:Xenarthra dbr:Interglacial dbr:Ratite dbr:Multituberculates dbr:Laurelia_novae-zelandiae dbr:Marsupials dbr:Subduction dbr:Climate dbr:Marsupial n17:Giant_moa.jpg dbr:Bounty_Trough dbr:Biodiversity_of_New_Caledonia dbr:Paleocene dbr:Pollen
dbo:wikiPageExternalLink
n4:books%3Fid=c8oZvgAACAAJ&q=ghosts+of+gondwana%7Ctitle=Ghosts n4:books%3Fid=mvc0kgAACAAJ&q=in+search+of+ancient+new+zealand%7Ctitle=In n4:books%3Fid=LIgbjgEACAAJ&q=a+continent+on+the+move%7Ctitle=A
owl:sameAs
wikidata:Q60739753 n15:9Ujni
dbp:wikiPageUsesTemplate
dbt:Clear dbt:Sfn dbt:Use_New_Zealand_English dbt:Location_map dbt:Use_dmy_dates dbt:Reflist dbt:Circa dbt:Convert dbt:Main dbt:Ma dbt:See_also dbt:Cite_book
dbo:thumbnail
n14:Zealandia_and_New_Zealand_90_ma_Gondwana.png?width=300
dbp:caption
Lake Taupo eruption, 186 AD
dbp:float
right
dbp:latDeg
38
dbp:latMin
43
dbp:lonDeg
176
dbp:lonMin
1
dbp:mark
Bullseye1.png
dbp:position
right
dbp:relief
1
dbp:width
100
dbp:latDir
S
dbp:lonDir
E
dbp:marksize
50
dbo:abstract
The natural history of New Zealand began when the landmass Zealandia broke away from the supercontinent Gondwana in the Cretaceous period. Before this time, Zealandia shared its past with Australia and Antarctica. Since this separation, the New Zealand landscape has evolved in physical isolation, although much of its current biota has more recent connections with species on other landmasses. The exclusively natural history of the country ended in about 1300 AD, when humans first settled, and the country's environmental history began. The period from 1300 AD to today coincides with the extinction of many of New Zealand's unique species that had evolved there. The break-up of Gondwana left the resulting continents, including Zealandia, with a shared ecology. Zealandia began to move away from the part of Gondwana which would become Australia and Antarctica approximately 85 million years ago (Ma). By about 70 Ma, the break up was complete. Zealandia has been moving northwards ever since, changing both in relief and climate. Most of the present biota of New Zealand has post-Gondwanan connections to species on other landmasses, but does include a few descendants of Gondwanan lineages, such as the Saint Bathans mammal. Overall, trans-oceanic dispersal has played a clear role in the formation of New Zealand's biota. Several elements of Gondwana biota are present in New Zealand today: predominantly plants, such as the podocarps and the southern beeches, but also distinctive insects, birds, frogs and the tuatara. In the Duntroonian stage of the Oligocene, the land area of Zealandia was at a minimum. It has been suggested that water covered all of it, but the consensus is that low-lying islands remained, perhaps a quarter of the modern land area of New Zealand.
prov:wasDerivedFrom
wikipedia-en:Natural_history_of_New_Zealand?oldid=1113355812&ns=0
dbo:wikiPageLength
32926
foaf:isPrimaryTopicOf
wikipedia-en:Natural_history_of_New_Zealand
Subject Item
dbr:Pre-Māori_settlement_of_New_Zealand_theories
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:Outline_of_New_Zealand
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
Subject Item
dbr:Geological_history_of_New_Zealand
dbo:wikiPageWikiLink
dbr:Natural_history_of_New_Zealand
dbo:wikiPageRedirects
dbr:Natural_history_of_New_Zealand
Subject Item
wikipedia-en:Natural_history_of_New_Zealand
foaf:primaryTopic
dbr:Natural_history_of_New_Zealand