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604 Revista de la Asociación Geológica Argentina 62 (4): 604-617 (2007) ANTARCTIC BIRDS (NEORNITHES) DURING THE CRETACEOUS-EOCENE TIMES Claudia TAMBUSSI and Carolina ACOSTA HOSPITALECHE Museo de La Plata, Paseo del Bosque s/nro, 1900 La Plata, and CONICET. E-mails: [email protected], [email protected] ABSTRACT: Antarctic fossil birds can be confidently assigned to modern orders and families, such as a goose-like anseriform, two loon-like and a serie- ma-like, all recorded before the K/T boundary at the López de Bertodano Fomation. Also, the discovery of a ratite and a phororhacids from the uppermost levels of the Submeseta Allomember (Late Eocene), suggests that West Antarctica was functional to dispersal routes obligate terrestrial birds. Representatives of Falconiformes Polyborinae, Ciconiiformes, Phoenicoteriformes, Charadriiformes, Pelagorni- tidae and Diomedeidae constitute the non-penguin avian assemblages of the Eocene of La Meseta Formation. Fifthteen Antarctic spe- cies of penguins have been described including the oldest penguin of West Antarctica, Croswallia unienwillia. The Anthropornis nordenskjoel- di Biozone (36.13 and 34.2 Ma, Late Eocene) is characterized by bearing one of the highest frequencies of penguin bones and the phos- patic brachiopod Lingula., together with remains of Gadiforms, sharks and primitive mysticete whales. Anthropornis nordenskjoeldi, Delphinornis gracilis, D. arctowski, Archaeospheniscus lopdelli, and Palaeeudyptes antarcticus are exclusively of the La Meseta Formation. Anthropornis nordenskjoeldi was evidently the largest penguin recorded at the James Ross Basin, whereas Delphinornis arctowski is the smallest, and include one of the worldwide highest morphological and taxonomic penguin diversity living sympatrically. The progressive climate cooling of the Eocene could have affected the penguin populations, because of climatic changes linked with habitat availability and food web processes. However, there is not available evidence about Antarctic penguins' evolution after the end of the Eocene. Keywords: Birds, Antarctica, Cretaceous, Paleogene. RESUMEN: Aves antàrticas (Neornithes) durante el lapso cretácico - eoceno. Las aves fósiles antárticas pueden ser asignadas a órdenes y familias vivientes, incluyendo restos de un Anseriformes que recuerda al ganso overo, dos colimbos y una supuesta seriema, todos registrados en sedimentos cretácicos de la Formación López de Bertodano. El hallaz- go de una ratites y un fororraco en los niveles más altos del Alomiembro Submeseta (Eoceno tardío) soporta la idea de que Antártida Oeste fue utilizada como ruta de dispersión por aves terrestres. Representantes de los Falconiformes Polyborinae, Ciconiiformes, Phoenicopteriformes, Charadriiformes, Pelagornitidae y Diomedeidae componen el conjunto de aves no-pingüinos registrados en los sedi- mentos Eocenos de la Formación La Meseta. Hasta el momento se describieron quince especies de pingüinos, incluyendo el más antiguo de los Sphenisciformes de Antártida Oeste, Croswallia unienwillia. Los pingüinos Anthropornis nordenskjoeldi, Delphinornis gracilis, D. arctowski, Archaeospheniscus lopdelli, y Palaeeudyptes antarcticus asociados con restos de tiburones, misticetos primitivos y Gadiformes se encuentran en la Biozona de Anthropornis nordenskjoeldi (36,13 and 34,2 Ma, Late Eocene). Estos niveles albergan una de las más grandes diversidades taxo- nómicas de pingüinos hasta ahora conocida. Anthropornis nordenskjoeldi fue sin dudas el pingüino más grande del Eoceno de Antártida mientras que en el otro extremo se ubica Delphinornis arctowski. Debido a que los cambios climáticos están ligados a la disponibilidad de habitat y de recursos alimenticios, el progresivo enfriamiento climático acaecido durante el Eoceno podría haber afectado a las poblacio- nes de pingüinos. Sin embargo, no tenemos evidencia acerca de la evolución de los pingüinos luego del Eoceno. Palabras clave: Aves, Antártida, Cretácico, Paleógeno. INTRODUCTION out in Seymour, James Ross and Vega Is- Recently, our understanding of the origins land have resulted in the discovery of signi- and evolution of Neornithes - all modern The James Ross Basin, at the Northern tip ficant vertebrate specimens that allow to birds-, has been dramatically influenced by of the Antarctic Peninsula, is one of the improve our comprehension of the evolu- both molecular and fossil researches. In- most important Early Cretaceous-early Pa- tionary history of Antarctic vertebrates, in deed, few neoavians from the end of the laeogene sedimentary sequences in the particular the one that regards to birds. Mesozoic are known (Hope 2002), but so- Southern Hemisphere (Francis et al. 2006a). However, despite intensive study of these me of them have been critical as factual evi- Fossil floras and both invertebrate and ver- areas in the past decades, there is still much dences of the presence of modern lineages tebrate faunas have provided clues to un- uncertainty about the exact composition of in the Cretaceous, and served as anchor derstand past climate and paleoenviron- the Cretaceous-Paleogene Antarctic avifau- points for the molecular clocks. This is the mental changes. Field expeditions carried na. case of the remarkable specimen of a mag- Antarctic birds (Neornithes) during the cretaceous-eocene times 605 pie-goose-like bird Vegavis iaai (Clarke et al. deposited in a back-arc setting relative to a and Cockburn iIslands, includes the Late 2005) to which we will refer below. volcanic arc through the Mid Mesozoic- Palaeocene Cross Valley Formation and the By other hand, the most significant fossil early Cenozoic times (Hathway 2000), du- richly fossiliferous Eocene La Meseta For- bird record from the James Ross Basin is ring subduction of the Pacific Ocean crust mation, both deposited in incised-valley that of penguins. Currently, fifteen penguin beneath Gondwana (Hayes et al. 2006). The settings. At its type section, in the central species have been described, and at least ten basin infilling consists of sandstones, silts- art of Seymour Island, the Cross Valley of which would have coexisted. Most pro- tones and conglomerates, and comprises Formation (Elliot and Trautman 1982) fills blematic is the assignment of many species three units: 1) the older Gustav Group (Ap- a steep-sided valley cut in the Lower Pa- from the Eocene of Seymour that are based tian-Coniacian) that comprises the Peder- laeocene Sobral Formation and older beds on non-comparable bones or different son, Lagrelius Point, Kotick Point, Whisky (Tambussi et al. 2005). parts of the skeleton (Tambussi et al. 2006, Bay and Hidden Lake formations, all confi- The youngest bird fauna is from La Meseta Tambussi et al. 2005). The recently publis- ned to the NW coast of James Ross Island Formation, which overlies the López de hed catalogue by Myrcha and coauthors (Crame et al. 2006); 2) the Marambio Group Bertodano Formation. This unit was inter- (2002) is a valuable source for the sphenis- (Coniacian-Maastrichtian), divided into preted as the filling of an incised-valley sys- cids described up to date. Santa Marta, Snow Hill Island and López tem and is the topmost exposed sector of The purpose of this paper is to review the de Bertodano formations (Pirrie et al. 1997) the sedimentary fill of the Late Jurassic- current state of knowledge of Antarctic and is exposed over most of the James Ross Tertiary James Ross Basin (Del Valle et al. Cretaceous-Paleogene avian fossils. Our ap- Basin. The latter group contains abundant 1992). It is composed of sandstones, muds- proach has four parts: 1) we describe and microfossils, as well as fossil plants, inverte- tones and conglomerates deposited during analyze the fossil continental birds; 2) we brates and vertebrates assemblages, profu- the Eocene in deltaic, estuarine and shallow report and analyze the fossil marine birds; sely studied in the last years; and 3) the marine settings (Marenssi et al. 1998 a, b ). 3) we discuss the bioestratigraphic impor- Seymour Island Group (Early Paleocene- From the base to the top, six units are dis- tance of the fossil penguin assemblage, and Late Eocene) that includes the Sobral, tinguished (Marenssi et al. 1998b): Valle de 4) we discuss the paleobiological significan- Cross Valley and La Meseta formations Las Focas, Acantilados, Campamento, Cu- ce of the Antarctic fossil birds. (Francis et al. 2006b). cullaea I, Cucullaea II and Submeseta Before developing each of these topics, The Late Cretaceous López de Bertodano Allomembers. The Valle de las Focas, Acan- some geological characteristics of James Formation contains the oldest Antarctic tilados and Campamento Allomembers Ross Basin will be considered. A more de- avian remains currently recorded (Case et al. constitute facies association I, composed by tailed account can be found in Francis et al. 2006a, Chatterjee 1989, Chatterjee 2002, a fine-grained sequence with mudstones (2006b). Chatterjee et al. 2006, Clarke et al. 2005, and very fine sandstones deposited in a del- The following institutional abbreviations Noriega and Tambussi 1995, 1996). Among ta front plain environment. Facies associa- are used in this paper: MLP Museo de La them, the anseriform Vegavis iaai was col- tion II includes the Cucullaea I, Cuccullaea Plata, MACN Museo Argentino de Ciencias lected at Cape Lamb, southwestern Vega II and the lower part of the Submeseta Naturales Bernardino Rivadavia, UCR Uni- Island (Western Antarctica), a well-known Allomembers, ranging from conglomeratic
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    762 ShortCommunications andCommentaries [Auk,Vol. 112 The Auk 112(3):762-767, 1995 Avian Premaxilla and Tarsometatarsusfrom the Uppermost Cretaceous of Montana ANDRZEJ ELZANOWSKIa AND MICHAEL K. BRETT-$URMAN2 •Departmentof VertebrateZoology, National Museum of NaturalHistory, SmithsonianInstitution, Washington, D.C. 20560, USA; and 2Departmentof Geology,George Washington University, Washington, D.C. 20052,USA Despitea variety of fragmentary,apparently neog- is rounded and smooth,and the sidesare very steep. nathousavian fossilsknown from the uppermostCre- The largest among the neurovascularforamina scat- taceousdeposits (Brodkorb 1963, Olson 1985, Olson tered on each side are two elongatedorsal foramina: and Parris 1987),we still lack even an approximate the vessel from the rostral one coursed rostrad, whereas idea of how many neognathouslineages survived be- the vesselfrom the caudalone apparentlybifurcated yond the Cretaceous/Tertiaryboundary. Most of the into a smaller rostral and a larger caudal branch. In Maastrichtian avian bones reveal a charadriiform or addition, a number of smaller openingsperforates transitional charadriiform-gruiform morphology, eachside of the symphysis. which may be plesiomorphicfor most (Olson 1985) The ventral surfaceof the premaxillarysymphysis but probably not all of the neognaths(Elzanowski is strongly concave(Fig. lc, d). There are no distinct 1995). Other than that, there is some fossil evidence neurovascularforamina on the ventral (palatal) sur- for the existence of loons in the Cretaceous(Olson face,with the possibleexception of one small opening 1992)and mostly indirect evidencefor the pre-Ter- on the left side. The palatal shelvesof the premaxilla tiary origins of the relict pelecaniforms(Phaethon- begin from the symphysialtip and graduallybroaden tidae and Fregatidae) and procellariiforms (Elza- caudally where each of them occupiesone-third of nowski and Gaiton 1991).
  • A Loon Leg (Aves, Gaviidae) with Crocodilian Tooth from the Late Oligocene of Germany

    A Loon Leg (Aves, Gaviidae) with Crocodilian Tooth from the Late Oligocene of Germany

    A Loon Leg (Aves, Gaviidae) with Crocodilian Tooth from the Late Oligocene of Germany GERALD MAYR1* AND MARKUS POSCHMANN2 1Forschungsinstitut Senckenberg, Sektion Ornithologie, Senckenberganlage 25, D-60325 Frankfurt am Main, Germany 2Generaldirektion Kulturelles Erbe RLP, Direktion Landesarchäologie, Referat Erdgeschichte, Große Langgasse 29, D-55116 Mainz, Germany *Corresponding author; E-mail: [email protected] Abstract.—The first late Oligocene fossil record of a loon (Gaviiformes) is described from the lacustrine depos- its of the German locality Enspel. The specimen is an isolated foot, which is associated with a crocodilian tooth. The fossil belongs to a species about half the size of the smallest extant loon, and is morphologically most similar to the Paleogene taxon Colymboides. In all probability it constitutes the prey remains of a crocodilian, which is of particular significance because the distribution ranges of loons and crocodilians hardly overlap today. The Enspel palaeocli- mate was warm-temperate and subtropical, and the Enspel specimen and other Paleogene fossils of gaviiform birds raise the, as yet, unanswered question of why loons largely disappeared from inland habitats of the warmer regions. Received 22 July 2008, accepted 30 December 2008. Key words.—Colymboides, crocodilian tooth, fossil waterbirds, Gaviiformes, palaeoecology. Waterbirds 32(3): 468-471, 2009 In recent years, the Enspel fossil site anglicus Lydekker, 1891 from late Eocene (Westerwald, Germany) has yielded several lacustrine deposits of England is represent- birds of late Oligocene age (MP 28, i.e. 24.7 ed by a coracoid (the holotype), and a re- million years ago; Mertz et al. 2007). The fos- ferred humerus and frontal portion of the siliferous sediments originated in a small skull (Harrison and Walker 1976).