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Habit and Ecology of the Petriellales, an Unusual Group of Seed Plants from the Triassic of Gondwana Author(S): Benjamin Bomfleur, Anne-Laure Decombeix, Andrew B

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Habit and Ecology of the Petriellales, an Unusual Group of Seed Plants from the Triassic of Gondwana Author(S): Benjamin Bomfleur, Anne-Laure Decombeix, Andrew B Habit and Ecology of the Petriellales, an Unusual Group of Seed Plants from the Triassic of Gondwana Author(s): Benjamin Bomfleur, Anne-Laure Decombeix, Andrew B. Schwendemann, Ignacio H. Escapa, Edith L. Taylor, Thomas N. Taylor, Stephen McLoughlin Source: International Journal of Plant Sciences, Vol. 175, No. 9 (November/December 2014), pp. 1062-1075 Published by: The University of Chicago Press Stable URL: http://www.jstor.org/stable/10.1086/678087 . Accessed: 08/12/2014 09:32 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The University of Chicago Press is collaborating with JSTOR to digitize, preserve and extend access to International Journal of Plant Sciences. http://www.jstor.org This content downloaded from 130.242.24.193 on Mon, 8 Dec 2014 09:32:01 AM All use subject to JSTOR Terms and Conditions Int. J. Plant Sci. 175(9):1062–1075. 2014. q 2014 by The University of Chicago. All rights reserved. 1058-5893/2014/17509-0008$15.00 DOI:10.1086/678087 HABIT AND ECOLOGY OF THE PETRIELLALES, AN UNUSUAL GROUP OF SEED PLANTS FROM THE TRIASSIC OF GONDWANA Benjamin Bomfleur,1,*,† Anne-Laure Decombeix,‡ Andrew B. Schwendemann,§ Ignacio H. Escapa,∥ Edith L. Taylor,† Thomas N. Taylor,† and Stephen McLoughlin* *Department of Palaeobiology, Swedish Museum of Natural History, PO Box 50007, SE-104 05 Stockholm, Sweden; †Department of Ecology and Evolutionary Biology and Biodiversity Institute, University of Kansas, Haworth Hall, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA; ‡Université Montpellier 2 and Centre National de la Recherche Scientifique, Unité Mixte de Recherche Botanique et Bioinformatique de l’Architecture des Plantes, Montpellier F-34000, France; §Department of Biology, Lander University, 320 Stanley Avenue, Greenwood, South Carolina 29649, USA; ∥Consejo Nacional de Investigaciones Científicas y Técnicas–Museo Paleontológico Egidio Feruglio, Trelew, Chubut 9100, Argentina Editor: Michael T. Dunn Premise of research. Well-preserved Triassic plant fossils from Antarctica yield insights into the physi- ology of plant growth under the seasonal light regimes of warm polar forests, a type of ecosystem without any modern analogue. Among the many well-known Triassic plants from Antarctica is the enigmatic Petriellaea triangulata, a dispersed seedpod structure that is considered a possible homologue of the angiosperm carpel. However, the morphology and physiology of the plants that produced these seedpods have so far remained largely elusive. Methodology. Here, we describe petriellalean stems and leaves in compression and anatomical preser- vation that enable a detailed interpretation of the physiology and ecology of these plants. Pivotal results. Our results indicate that the Petriellales were diminutive, evergreen, shade-adapted pe- rennial shrubs that colonized the understory of the deciduous forest biome of polar Gondwana. This life form is very unlike that of any other known seed-plant group of that time. By contrast, it fits remarkably well into the “dark and disturbed” niche that some authors considered to have sheltered the rise of the flowering plants some 100 Myr later. Conclusions. The hitherto enigmatic Petriellales are now among the most comprehensively reconstructed groups of extinct seed plants and emerge as promising candidates for elucidating the mysterious origin of the angiosperms. Keywords: Petriellales, gymnosperms, Triassic, paleoecology, polar forests, Antarctica. Introduction today exposed in the Transantarctic Mountains; these suc- cessions have yielded abundant compression-fossil assem- Since plant life conquered land in the early Paleozoic, blages as well as silicified peat deposits that contain plant global climates have been generally much warmer than today, remains in exquisite anatomical detail. The rich and well- enabling the terrestrial vegetation to spread far into polar preserved plant-fossil record from the Triassic of Antarctica latitudes (Seward 1914; Spicer and Chapman 1990; Taylor provides insights into the physiology of plant growth under and Taylor 1990; Cantrill and Poole 2012). In the Triassic the strongly seasonal light regimes of a warm polar forest greenhouse world, lush temperate forests covered large parts biome—a type of ecosystem without any modern analogue of the high-latitude regions of the Gondwanan supercontinent (Taylor and Taylor 1990; Escapa et al. 2011; Cantrill and (Taylor and Taylor 1990; Escapa et al. 2011; Cantrill and Poole 2012). Poole 2012). Sedimentary successions of an extensive fluvial Among the numerous and, in many cases, well-studied drainage system that transected this polar forest biome are Triassic plants from Antarctica are the Petriellales—an order of enigmatic seed plants that was established with the de- scription of a peculiar type of dispersed seedpod structure in the famous silicified peat deposit from Fremouw Peak, East 1 fl Author for correspondence; e-mail: benjamin.bom [email protected]. Antarctica (Taylor and Taylor 1987; Taylor et al. 1994). Manuscript received April 2014; revised manuscript received July 2014; Anatomical details led some authors to consider Petriellaea electronically published October 28, 2014. triangulata a possible homologue of the angiosperm carpel 1062 This content downloaded from 130.242.24.193 on Mon, 8 Dec 2014 09:32:01 AM All use subject to JSTOR Terms and Conditions BOMFLEUR ET AL.—HABIT AND ECOLOGY OF THE PETRIELLALES 1063 (see Frohlich 2003; Frohlich and Chase 2007; Doyle 2008). and CB545) of the famous permineralized peat deposit from Compression fossils of similar cupulate structures (Kannas- the uppermost Fremouw Formation exposed at a col on the koppia) and of associated pollen organs (Kannaskoppianthus) north side of Fremouw Peak in the Beardmore Glacier area were later found in organic connection to small stems with of the central Transantarctic Mountains (fig. 1). The exact attached leaves in Triassic deposits from South Africa (An- age of this deposit remains uncertain. Following a palyno- derson and Anderson 2003) and Australia (Holmes and An- logical analysis by Farabee et al. (1990), the permineralized derson 2005). The leaves (Rochipteris, Kannaskoppifolia) are peat deposit has conventionally been assigned to the Anisian apetiolate, arise helically, and have a wedge-shaped, spread- (early Middle Triassic). This dating was based on the as- ing, variably dissected lamina and distinctive anastomosing sumption that the occurrence of Aratrisporites parvispino- venation (Anderson and Anderson 2003; Barone-Nugent sus and an undetermined species of Protohaploxypinus (i.e., et al. 2003; Holmes and Anderson 2005). Anderson and An- Protohaploxypinus cf. microcorpus) in a palynological sam- derson (2003, p. 288) reconstructed the South African fossils ple from the permineralized peat would indicate an age no as the remains of small, erect plants that they tentatively in- younger than Anisian (early Middle Triassic). However, A. terpreted as herbaceous pioneering shrublets or climbers (An- parvispinosus and Protohaploxypinus species also occur in derson and Anderson 2003, p. 294). younger deposits (e.g., Helby et al. 1987). By contrast, other Here, we present the first discoveries of petriellalean com- palynological studies (Fasola 1974; Kyle and Schopf 1982) pression fossils from Antarctica. Information about the dis- place the uppermost part of the Fremouw Formation, which tinctive morphology of petriellalean stems and leaves enabled includes the silicified peat deposits, into subzone C of the us to identify the corresponding anatomically preserved parts informal Alisporites zone (Kyle 1977), indicating a late La- of these plants in the silicified peat deposit. Detailed analysis dinian (latest Middle Triassic) or possibly Carnian (early Late of morphological, anatomical, and taphonomic features of Triassic) age. We consider this latter assignment to be more these new Antarctic fossils reveals that the Petriellales had likely. indeed established a habit and life strategy that are unique All material is housed in the Paleobotanical Collections of among all known seed-plant groups of the time and much the University of Kansas in Lawrence. Permineralized peat more reminiscent of early angiosperms. blocks were prepared, analyzed, and photographed following standard paleobotanical procedures (see, e.g., Galtier and Material and Methods Phillips 1999). In the Paleobotanical Collections of the Department of Ecol- Systematic Description ogy and Evolutionary History and Biodiversity Institute at the University of Kansas, Lawrence (KUPB), petriellalean fossils Order—Petriellales Taylor et al. 1994 occur in three plant-fossil assemblages from different sites in the Transantarctic Mountains (fig. 1). More or less complete Family—Petriellaceae Taylor et al. 1994 remains of more than 20 leaves plus abundant leaf fragments occur on 10 hand specimens (KUPB T-234, 256, 257, 577, Genus—Rochipteris Herbst et al. 2001, emend. nov. 581, 584, 585, 634, 661, 663) in a compression assemblage from plant level 2 (in E. L. Taylor et al. 1990; Boucher et al. Type species. Rochipteris lacerata (Arber) Herbst
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