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Taxonomic revision of Eocene Antarctic penguins based on tarsometatarsal morphology

TLDR
Gradual cooling of climate, changes of environment and trophic relationships, that lasted several millions years, were most probably responsible for the intense speciation and taxonomic diversification of the Middle-Late Eocene La Meseta penguins.
Abstract
Eocene penguin remains from Seymour Island (Antarctica) are so far the old− est−known record of extinct Sphenisciformes. Rich Argentine and Polish collections of pen− guin bones from the La Meseta Formation are taxonomically revised on tarsometatarsal morphology. Two genera and four species are erected: Mesetaornis polaris gen. et sp. n., Marambiornis exilis gen. et sp. n., Delphinornis arctowskii sp. n. and D. gracilis sp. n. Moreover, the diagnoses of already described species: Anthropornis nordenskjoeldi, A. grandis, Palaeeudyptes klekowskii, P. gunnari, Archaeospheniscus wimani and Delphi− nornis larseni are revised as well. Gradual cooling of climate, changes of environment and trophic relationships, that lasted several millions years, were most probably responsible for the intense speciation and taxonomic diversification of the Middle-Late Eocene La Meseta penguins.

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Early Penguin Fossils, Plus Mitochondrial Genomes, Calibrate Avian Evolution

TL;DR: A test for events around the Late Cretaceous is reported by describing the earliest penguin fossils, analyzing complete mitochondrial genomes from an albatross, a petrel, and a loon, and describing the gradual decline of pterosaurs at the same time modern birds radiate.
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The phylogeny of the living and fossil Sphenisciformes (penguins)

TL;DR: The results do not support an expansion of the Spheniscidae from a cooling Continental Antarctica, but instead suggest those species that currently breed in that area are the descendants of colonizers from the Subantarctic.
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Phylogenetic analysis of pelecaniformes (aves) based on osteological data: implications for waterbird phylogeny and fossil calibration studies.

TL;DR: Relationships of extant pelecaniforms inferred from morphology are more congruent with molecular phylogenies than previously assumed, though notable conflicts remain.
Journal Article

First Cenozoic glaciers in West Antarctica

TL;DR: In this paper, a terrestrial, valley-type tillite up to 65 metres thick was revealed between two basaltic lava sequences in the Eocene-Oligocene Point Thomas Formation at Herve Cove - Breccia Crag in Admiralty Bay, King George Island, South Shetland Islands.
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The Basal Penguin (Aves: Sphenisciformes) Perudyptes devriesi and a Phylogenetic Evaluation of the Penguin Fossil Record

TL;DR: These two species, known from relatively complete partial skeletons, are the oldest crown clade penguin fossils and represent well-corroborated temporal calibration points for the Spheniscus-Eudyptula divergence and Megadyptes-EUDyptes divergence, respectively.
References
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Journal Article

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W. M. Goodchild
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Journal ArticleDOI

Catalogue of Fossil Birds Pierce Brodkorb

Robert W. Storer
- 01 Oct 1965 - 
Journal ArticleDOI

Dispersal, Vicariance, and the Late Cretaceous to Early Tertiary Land Mammal Biogeography from South America to Australia

TL;DR: A review of paleontological, phyletic, geophysical, and climatic evidence leads to a new scenario of land mammal dispersal among South America, Antarctica, and Australia in the Late Cretaceous to early Tertiary epochs as mentioned in this paper.
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