Phytogeographic and Phylogenetic History of the Genus Nothofagus Bl. (Fagaceae) in the Southern Hemisphere

The genus Nothofagus Bl. (Fagaceae) is one of the representative tree genera in the temperate forests of the southern hemisphere, and its phytogeographic history has been in controversy regarding the origin and dispersal route. Based on a recent collection from the Tertiary of southern Chile, all th...

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Main Author: Tanai, Toshimasa
Format: Article in Journal/Newspaper
Language:English
Published: 北海道大学
Subjects:
450
Online Access:http://hdl.handle.net/2115/36741
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spelling fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/36741 2023-05-15T13:55:39+02:00 Phytogeographic and Phylogenetic History of the Genus Nothofagus Bl. (Fagaceae) in the Southern Hemisphere Tanai, Toshimasa http://hdl.handle.net/2115/36741 eng eng 北海道大学 http://hdl.handle.net/2115/36741 北海道大学理学部紀要, 21(4): 505-582 450 bulletin (article) fthokunivhus 2022-11-18T01:01:39Z The genus Nothofagus Bl. (Fagaceae) is one of the representative tree genera in the temperate forests of the southern hemisphere, and its phytogeographic history has been in controversy regarding the origin and dispersal route. Based on a recent collection from the Tertiary of southern Chile, all the previously-described species of Nothofagus or Nothofagus-like leaf fossils from South America and West Antarctica were reinvestigated, and compared with leaf architecture of nearly all the extant species of the genus in their phylogenetic relationships. The investigation of straligraphic and areal distribution of fossils (leaves, wood and pollen) in South America reveals that Nothofagus gradually dispersed northward from the Antarctic region since Late Cretaceous to Miocene time. Leaves and pollen occur abundantly with various species in the Oligocene and the Lower Miocene of the Patagonia region compared with paucity in the same horizons of northern region. This northward dispersal corresponds with the considerably descreasing temperature since Late Eocene age, which was suggested by oxygen isotope studies of sub-antarctic marine animal fossils. The bibliographic survey of fossil records of Nothofagus leaves and pollen in other southern continents and deep-sea sediments further substantiated a conclusion that this genus seems to have been in southern origin during Late Cretaceous time. The comparison of leaf architecture with all the morphological characters of extant species allows that 36 extant species of Nothofagus are classified into five groups. A scheme of phylogenetic relationships of these extant species is proposed here, and it is consistent with breakup sequences of the Gondwanaland that is generally accepted by most workers. Article in Journal/Newspaper Antarc* Antarctic Antarctica West Antarctica Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Antarctic Patagonia The Antarctic West Antarctica
institution Open Polar
collection Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP)
op_collection_id fthokunivhus
language English
topic 450
spellingShingle 450
Tanai, Toshimasa
Phytogeographic and Phylogenetic History of the Genus Nothofagus Bl. (Fagaceae) in the Southern Hemisphere
topic_facet 450
description The genus Nothofagus Bl. (Fagaceae) is one of the representative tree genera in the temperate forests of the southern hemisphere, and its phytogeographic history has been in controversy regarding the origin and dispersal route. Based on a recent collection from the Tertiary of southern Chile, all the previously-described species of Nothofagus or Nothofagus-like leaf fossils from South America and West Antarctica were reinvestigated, and compared with leaf architecture of nearly all the extant species of the genus in their phylogenetic relationships. The investigation of straligraphic and areal distribution of fossils (leaves, wood and pollen) in South America reveals that Nothofagus gradually dispersed northward from the Antarctic region since Late Cretaceous to Miocene time. Leaves and pollen occur abundantly with various species in the Oligocene and the Lower Miocene of the Patagonia region compared with paucity in the same horizons of northern region. This northward dispersal corresponds with the considerably descreasing temperature since Late Eocene age, which was suggested by oxygen isotope studies of sub-antarctic marine animal fossils. The bibliographic survey of fossil records of Nothofagus leaves and pollen in other southern continents and deep-sea sediments further substantiated a conclusion that this genus seems to have been in southern origin during Late Cretaceous time. The comparison of leaf architecture with all the morphological characters of extant species allows that 36 extant species of Nothofagus are classified into five groups. A scheme of phylogenetic relationships of these extant species is proposed here, and it is consistent with breakup sequences of the Gondwanaland that is generally accepted by most workers.
format Article in Journal/Newspaper
author Tanai, Toshimasa
author_facet Tanai, Toshimasa
author_sort Tanai, Toshimasa
title Phytogeographic and Phylogenetic History of the Genus Nothofagus Bl. (Fagaceae) in the Southern Hemisphere
title_short Phytogeographic and Phylogenetic History of the Genus Nothofagus Bl. (Fagaceae) in the Southern Hemisphere
title_full Phytogeographic and Phylogenetic History of the Genus Nothofagus Bl. (Fagaceae) in the Southern Hemisphere
title_fullStr Phytogeographic and Phylogenetic History of the Genus Nothofagus Bl. (Fagaceae) in the Southern Hemisphere
title_full_unstemmed Phytogeographic and Phylogenetic History of the Genus Nothofagus Bl. (Fagaceae) in the Southern Hemisphere
title_sort phytogeographic and phylogenetic history of the genus nothofagus bl. (fagaceae) in the southern hemisphere
publisher 北海道大学
url http://hdl.handle.net/2115/36741
geographic Antarctic
Patagonia
The Antarctic
West Antarctica
geographic_facet Antarctic
Patagonia
The Antarctic
West Antarctica
genre Antarc*
Antarctic
Antarctica
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
West Antarctica
op_relation http://hdl.handle.net/2115/36741
北海道大学理学部紀要, 21(4): 505-582
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