Palmoxylon </Emphasis> from the Deccan Intertrappean Beds

Total Page:16

File Type:pdf, Size:1020Kb

Palmoxylon </Emphasis> from the Deccan Intertrappean Beds A NEW SPECIES OF PALMOXYLON FROM THE DECCAN INTERTRAPPEAN BEDS BY MISS VIMALA K. MENON (Department of Botany, University of Lucknow) Received October 3, 1963 (Commtmieated by Prof. L. Narayana Rao, v.A.ac.) INTRODUCTION THE specimen described here is one of the many fragments of silicified palm woods collected from Mohgaon Kalan area, Madhya Pradesh, a locality from which a number of petrified palm woods have been described. The specimen is fragmentary but measuring about 6- 5 cm. in length and 3 -4 cm. in breadth. The preservation is not quite satisfactory, yet the arrangement of the bundles in the different zones of the wood is very clear to the naked eye on the polished surface of the specimen. The specimen is brownish-yellow in colour. In thin sections the yellow portions look white. ANATOMICAL DESCRIPTIONS Transverse sections of the specimen show three distinct zones--the Dermal, Sub-dermal and Central (Plate II, Photo 1). Fortunately, a small portion of th~ cortex also is preserved on the outside of these zones. Thin sections of the cortical region show mainly fibrous bundles. They are of varying sizes and irregularly distributed (Fig. 1). The ground tissue is compactly arranged, with thin-walled cells. Dermal zone consists of fibrovascular bundles regularly orientated and closely placed (Fig. 2 ; Plate II, P~oto 2). The row of bundles just belo wthecor- tex isvery small in size and are more orless round to oval inshape (Figs. 3-5). The rest of the bundles are elongated (Figs. 6-13). In between these elongated bundles are seen some smaller bundles (Figs. 14 and 15). The frequency of the bundles is 245 to 320 per cm. ~ and they are about 0-2-0-5ram. in diameter. The bundles are Very crowded, so that they leave very little space for the ground tissue. And even this.is very compact in nature with some intercellular spaces. Thef/v ratio in the main bundles is about 0"5/1-1.4/1. The auricular lobes are round and the median sinus is concave. Phloem is preserved in some of the bundles. The vascular part consists mostly of 77 78 Miss VIMALA K, MENON 'i¢ 21 1 25 FIGS. 1-25. Fig. 1. Transverse section of the cortical region showing the fibrou bundles and the ground tissue, x 56. fb, fibrous bundles. Fig. 2. Distribution of th~ fibrovasculat bundles in the dermal zone, x 36. eb, crushed bundle. Figs. 3-5. Smaller bundles in tho region below the cortex, ×60. Figs. 6-15. Different kinds of bundles in the dermal zone, x60. Fig. 16. Distribution of the fibrovascular bundles in the sub-dermal zone, x 36. Fi~. 17-23. Different kinds of bundles in the sub-dermal zone, x 60. Fig. 24. One fibrovascular bundle of the sub-dermal zone showing the grouped xylem vessels, x 60. Fig. 25. One fused bundl~ )howi~ tho fmio= on tl~ vascul~ part, x C30. A New Speoies of Palmoxylon from the Deccan Intertrappean Beds 79 one main xylem vessel (Figs. 6-10) but sometimes a pair of vessels lying side by side (Figs. 11 and 12). Protoxylem is present. The vessels are ccmpletely excluded or are outside the median sinus. There is no radiating or tabular parenchyma seen around the fibrovascular bundles. Sub-dermal zone.--The majority of the fibrovascular bundles are regularly orientated and are less densely crowded (Fig. 16; Plate II, Fhoto 3). They are 150-170 per cm. °- and are of different sizes and ,~hapes (Figs. 17-23). The bundles are 0" 3-0.6 mm. in diameter and their fly ratio varies from 0.4/1-1/1. The auricular lobes are mostly round, the median sinus is concave to somewhat fiat (Figs. 17-23). Usually, there are two big, circular to oval main vessels, excluded, placed side by side in the vascular parts of the bundles (Figs. 18-23). Some of the bundles consist of a numl:er of xylem vessels grouped tcgelher (Fig. 24). This type of bundles are seen in all the three zones. Smaller rounded bundles occur in between the olher main bundles (Fig. 22). Radiat- ing and tabular parenchyma cells surrounding the bundles are totally absent. Here and there are found some fused bundles. Their fusion takes place either in the sclerenchyma parts or in the vascular parts (Figs. 25 and 26). Leaf-traces are often found in this zone. They are bigger lhan the main bundles (Fig. 27). Central zone is distinguished by the irregular orientation of the fibre- vascular bundles (Fig. 28 ; Plate II, Fhoto 4) and lhey are far apart from each other. They are 80--125 per cm. 2 and are 0.5-0-8 ram. in diameter. The varying form of bundles is seen in Figs. 29-33. The fly rati 9 of the bundles is 0.3/1-0.8/1. The median sinus is somewhat concave and auricular lobes are round. Rounded, excluded, paired vessels occur more commonly in the vascular parts of the bundles (Figs. 30, 31 and 33; Plate III, Photo 5). In between the big bundles there occur occasionally a few small fibrovascular bundles. Radiating or tabular parenchyma cells are conspicuous by their absence. Leaf-trace bundles are very common here (Fig. 34). Fibrous bundles are present only in the cortex. They are altogether absent in the other three zones. Stegmata also have not been observed in any of the fibrovascular bundles. Phloem is preserved in most of the bundles in all the three zones. A more or less triangular-shaped phloem cavity is clearly seen in the bundles in which the phloem is not preserved, 80 Mms VI~LA K. MENOI~ dsc xy i Y ' ii::!!i!ii FIos. 26-35. Fig. 26. One fused bundle showing the fusion on the sclerenchyma part, x75. Fig. 27. One leaf-trace bundle of the sub-dermal zone, × 75. Pxy, protoxylem. Fig. 28. Distribution of the bundles in the central zone, x45. Fig. 29-32. Different types of bundles in the central zone, x 75. Fig. 33. One fibrovascular bundle of the central zone showing all the tissues, x75, dse, dorsal sclerenchyma; mxy, metaxylem; P, parenchyma; ph, phloem; pxy, protoxylem. Fig. 34. One leaf-trace bundle of the central zone, x?5. pxj,, "protoxylern. Fi8. 35, A poltion of the ground tissue in the central,zone, x75, A New Species of Paimoxylon from the Deccan Intertrappean Beds $1 The ground tissue is compact throughout the wood (Fig. 35). The cells are thin-walled, oval to rounded in shape with slight intercellular spaces occasionally seen in between them. In the longitudinal sections these cells are seen to be placed contiguously in vertical rows (Plate III, Photo 6) as in other palm woods. There are some special type of cells present in the ground tissue (Plate II, Photos 2-4). The bad preservation makes it difficult to say what they are. They are mostly single-celled structures, but sometimes a chain of five or six cells joined together are also seen. Some of them show bar-like thicken- ings. The nature of these cells could not be determined. But they may be comparable to idioblasts as reported in the case of Palmoxylon sclerodermum by Sahni (1943). Longitudinal sections show the pitting of the xylem vessels is of the multiseriate scalariform as well as typical helical types (Plate III, Photo 6). The perforated end-walls are obliquely placed and show a series of widely spaced parallel bars of thickening (Plate III, Photo 7). DISCUSSION Quite a large number of palm woods have been described from the Deccan Intertrappean beds by several authors (Sahni, 1931, 1943, 1946; Rode, 1933; Shukla, 1939, 1946; Ramanujam, 1953, 1958; Lakhanpal, 1955; Mahabale, 1958; Prakash, 1958; 1961; Rao and Menon, 1962, 1963). The characters of all these palms have been incorporated in a tabular form (Rao and Menon, 1963). The specimen described in the present paper shares some character or other with each one of the species in Table I. The absence or presence of fibrous bundles, stegmata, radiating or tabular parenchyma, posterior sclerenchyma, are some such characters--which may be considered as comparatively unimportant. But a closer comparison can be possible with Palmoxylon puratanam, Palmoxylon narayanai and Palmoxylon mahesb- warii. The specimen described in this paper resembles the above-mentioned three species in a few of the characters, but differs from them in some of the importan t characters, like frequency of the bundles in the various zones of the wood ; fly ratio of the bundles ; and the diameter and nature of the bundles. The number of bundles per cm. ~ in this species is greater than in P. puratanam, P. narayanai and the bundles in the dermal zone of P. maheshwarff but lesser than those in the sub-dermal and ~entral zones. The fly ratio of P. puratanam and P. narayanai is greater than the fly ratio of the specimen described here, while f/v ratio of P. maheshwarii is lesser. As far as the nature, shape and type of the fibrovascular bundles are concerned these four species are quite different from each other. This can be noted easily from the figures and 82 Mms VI~,LA K. M~oN TABLE Diameter Base of the Name of the Frequency f]~ ratio Palmoxylon of of the [ dorsal No. Cortex of the bundles [ sclersn- species the bundles bundles (inmm.) [ chyma Palmoxylom Imperfectly preserved D-80-100/cxa.* D-4/1 D--0.8- Rounded puratanam thin-walled paten- SI~-7.~/cm. t SD-3/2- 0-5 cordate (Ramanujam. chyma calls. Nume- C-20-25/cm. s 1½/1 SD-0.95- median C.
Recommended publications
  • Palmoxylon Phytelephantoides Sp.Nov.- a New Fossil Palm from the Deccan Intertrappean Beds of Umaria, Madhya Pradesh, India
    International Journal of Advanced Scientific Research and Management, Volume 4 Issue 6, June 2019 www.ijasrm.com ISSN 2455-6378 Palmoxylon phytelephantoides sp.nov.- A New Fossil Palm from the Deccan Intertrappean Beds of Umaria, Madhya Pradesh, India 1 2 3 S.V. Chate , S.D. Bonde , P.G. Gamre 1Department of Botany, Shivaji Mahavidyalaya Udgir, Dist-Latur, Maharashtra, India. 2,3 Palaeobiology Division,Agharkar Research Institute, Pune, Maharashtra,India. Abstract monocotyledons, the Arecaceae shows by far the The present paper deals with a new petrified palm richest fossil record, and there is an extensive stem having root matrix under the organ genus literature available. Though, fossil material often Palamoxylon (Palmoxylon phytelephantoides lacks sufficient diagnostic detail to allow reasonable association with living palm taxa beyond, or even to, sp. nov.) from Deccan Intertrappean Beds of subfamilial level. However, many fossil genera and Umaria, Madhya Pradesh, India with its numerous species have been described. phytogeographical significance. Detailed anatomical Umaria is one of the well-known plant fossil locality investigations suggest its resemblance with the belongs to Deccan Intertrappean beds which have Phytelephantoid palm, Phytelephas Ruiz & Pavon. been dated 65 million years old (Krishnan, Occurrence of fossils of Phytelephas in the Deccan Intertrappean beds of India and their present 1973). Fossils are scattered and widely spread over distribution in South America and Panama has a in a large area of Umaria, Dindori and Mandla phytogeographical significance. Fossil stem of districts of Madhya Pradesh, India. Records of Phytelephas (P. sewardii) and a seed (P. olssoni fossils, including a large number of plant organs such Brown,) has been reported from Central America as roots, stems, leaves, rhizomes, fruits, seeds, and where extant Phytelephas grows naturally.
    [Show full text]
  • The Cretaceous System in Central Sierra County, New Mexico
    The Cretaceous System in central Sierra County, New Mexico Spencer G. Lucas, New Mexico Museum of Natural History, Albuquerque, NM 87104, [email protected] W. John Nelson, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Karl Krainer, Institute of Geology, Innsbruck University, Innsbruck, A-6020 Austria, [email protected] Scott D. Elrick, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Abstract (part of the Dakota Formation, Campana (Fig. 1). This is the most extensive outcrop Member of the Tres Hermanos Formation, area of Cretaceous rocks in southern New Upper Cretaceous sedimentary rocks are Flying Eagle Canyon Formation, Ash Canyon Mexico, and the exposed Cretaceous sec- Formation, and the entire McRae Group). A exposed in central Sierra County, southern tion is very thick, at about 2.5 km. First comprehensive understanding of the Cretaceous New Mexico, in the Fra Cristobal Mountains, recognized in 1860, these Cretaceous Caballo Mountains and in the topographically strata in Sierra County allows a more detailed inter- pretation of local geologic events in the context strata have been the subject of diverse, but low Cutter sag between the two ranges. The ~2.5 generally restricted, studies for more than km thick Cretaceous section is assigned to the of broad, transgressive-regressive (T-R) cycles of 150 years. (ascending order) Dakota Formation (locally deposition in the Western Interior Seaway, and includes the Oak Canyon [?] and Paguate also in terms of Laramide orogenic
    [Show full text]
  • UNDERGRADUATE PROGRAMME in BOTANY (B.Sc. BOTANY - MODEL I)
    SACRED HEART COLLEGE (AUTONOMOUS), THEVARA KOCHI, KERALA, 682013 CURRICULUM AND SYLLABI CHOICE BASED CREDIT AND SEMESTER SYSTEM (CBCSS) UNDERGRADUATE PROGRAMME IN BOTANY (B.Sc. BOTANY - MODEL I) INTRODUCED FROM 2019 ADMISSION ONWARDS BOARD OF STUDIES IN BOTANY Sacred Heart College, Thevara, Kochi, Kerala B.Sc. Botany Programme – Curriculum and Syllabi 2019 CONTENTS Sl. No. Page No. 1 Forward 03 2 Members of the BoS in Botany 05 3 Curriculum 06 4 Grievance Redressal Mechanism 24 5 B.Sc. Botany Programme Outcomes (POs) 25 6 Syllabus of Core Courses 26 7 Pattern of Question Papers 77 8 Model Question Papers Core (Theory) 78 9 Model Question Papers Core (Practical) 92 10 Syllabus of Complementary Courses 104 11 Model Question Papers (Compl. Theory) 113 12 Model Question Papers (Compl. Practical) 117 BoS in Botany, Sacred Heart College, Thevara : Page 2 B.Sc. Botany Programme – Curriculum and Syllabi 2019 FORWORD Science is a study dealing with a body of facts or truths systematically and the base of all developments in the world is because of practical application of science, i.e. technology. The creation of a scientific thinking in society necessitates proper education and guidance. In order to achieve this, one must update the developments in every field of science. To achieve this goal, the curriculum of every programme in science should be revised frequently to incorporate the recent advances in science. In line with the changes in higher education, the state of Kerala had introduced the autonomy in its 13 selected colleges in 2014. Exercising the opportune occasion of autonomy, the dept.
    [Show full text]
  • Late Cretaceous Palm Stem Palmoxylon Lametaei Sp. Nov. from Bhisi Village, Maharashtra, India
    Revista Mexicana de Ciencias Geológicas,Palmoxylon v. 28, núm. lametaei1, 2011, p.sp. 1-9 nov., Maharashtra, India 1 Late Cretaceous palm stem Palmoxylon lametaei sp. nov. from Bhisi Village, Maharashtra, India Debi Dutta1,*, Krishna Ambwani1, and Emilio Estrada-Ruiz2, ** 1 Geology Department, Lucknow University, Lucknow-226007, India. 2 Unidad Académica en Ciencias de la Tierra, Universidad Autónoma de Guerrero, Ex Hacienda de San Juan Bautista, 40323 Taxco El Viejo, Guerrero, Mexico. * [email protected], ** [email protected] . ABSTRACT A new fossil palm trunk Palmoxylon lametaei sp. nov. is described from the Lameta Formation (Upper Cretaceous) of Bhisi area of Nand inland basin, Nagpur District, Maharashtra, India. The stem is well preserved revealing all the anatomical features identifiable to the modern arecoid palm (Phoenix). The fossil plant is characterized by the presence of cortical, dermal, sub-dermal and central zones with profuse roots in the bark region, indicating a basal part of the stem. Presence of fibrous and diminutive bundles only in the outer part of the stem is significant while a gradual transformation from compact to lacunar condition of ground tissue from outer to inner part of the stem suggests that the plants thrived under aquatic environment. Key words: Arecaceae, Palmoxylon, Lameta Formation, Upper Cretaceous, India. RESUMEN Un nuevo estípite de palmera fósil Palmoxylon lametaei sp. nov. se describe para la Formación Lameta (Cretácico Superior) dentro del área de Bhisi de la cuenca Nand, Distrito Nagpur, Maharashtra, India. El tallo está bien preservado y revela todas las características anatómicas para la identificación con palmas modernas (Phoenix). La planta fósil se caracteriza por la presencia de corteza, una zona dermal, zona subdermal y central, con raíces abundantes en la región de la corteza, lo que indica una parte basal del tallo.
    [Show full text]
  • Early Eocene Arecoid Palm Wood, Palmoxylon Vastanensis N
    Journal of the Palaeontological Society of India ISSN 0522-9630 Volume 58(1), June 2013: 115-123 EARLY EOCENE ARECOID PALM WOOD, PALMOXYLON VASTANENSIS N. SP. FROM VASTAN LIGNITE, GUJARAT, INDIA: ITS PALAEOENVIRONMENTAL IMPLICATIONS M. PRASAD ¹, H. SINGH ¹, S. K. SINGH ¹, DEBI MUKHERJEE ² and EMILIO ESTRADA RUIZ3 1.BIRBAL SAHNI INSTITUTE OF PALAEOBOTANY, 53, UNIVERSITY ROAD, LUCKNOW- 226007, INDIA. 2. CENTRE OF ADVANCE STUDY IN GEOLOGY, LUCKNOW UNIVERSITY, LUCKNOW, 226007, U.P. INDIA. 3.UNITED ACADEMICAEN CIENCIASDELA TIERRAUNIVERSITDAD AUTONOMADE GUERRERO EX HACIENDA DE SAN JUAN BAUSTINA, 40323, TAXCO EL VIEJO, MEXICO. Corresponding author: E-mails: ¹[email protected], ² [email protected] ABSTRACT A new species of fossil palm wood, Palmoxylon vastanensis is reported and described from the Vastan Lignite Mine, Surat, Gujarat, India. The fossil wood is characterized by highly lacunar ground tissue with very large air spaces indicating that plants were growing in an aquatic or the marshy environment. A detailed anatomical study revealed its affinities with the extant arecoid taxa belonging to the family Arecaceae. Among them, it closely resembles Areca catechu as both fossil and living species possess similar anatomical features such as highly lacunar ground tissue, reniform, dorsal sclerenchymatous sheath of the fibrovascular bundles with the frequency of 30-35 per cm². Based on the anatomical characters of the fossil and present day ecology of its modern equivalent, the palaeoenvironmental implications have been discussed. Keywords: Palmoxylon vastanensis n. sp., Arecaceae, anatomy, palaeoenvironment, Vastan Lignite, Lower Eocene, Gujarat, India INTRODUCTION the Gulf of Cambay (Fig.1). The Vastan opencast lignite mine is The subsurface beds of the Lower Cambay Shale exposed situated about 29 km NE of Surat.
    [Show full text]
  • Synoptic Taxonomy of Major Fossil Groups
    APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida
    [Show full text]
  • Fossils in Oregon: a Collection of Reprints
    BULLETIN 92 FOSSILS IN OREGON A.: C.P L l EC T1 0 N 0 F R-EPR l N T S F..«OM lft� Ol£ Bl N STATE OF OREGON DE PARTMENT OF GEOLOGY AND MINERAL INDUSTRIES 1069 State Office Building, Portland, Oregon 97201 BULLETIN 92 FOSSILS IN OREGON A COLLECTION OF REPRINTS FROM THE ORE BIN Margaret L. Steere, Editor 1977 GOVERNING BOARD R . W. deWeese, Chairman Portland STATE GEOLOGIST Leeanne Mac Co 11 Portland Ralph S. Mason Robert W. Doty Talent PALEONTOLOGICAL TIME CHART FOR OREGON ERA I PERIOD EPOCH CHARACTERISTIC PLANTS AND ANIMALS AGE* HOLOCENE Plant and animal remains: unfossilized. ".11- Mastodons and giant beavers in Willamette Valley. PLEISTOCENE Camels and horses in grasslands east of Cascade Range. >- Fresh-water fish in pl�vial lakes of south-central Oregon. <("" z: ?-3- LU"" Sea shell animals along Curry County coast. >-- <( Horses, camels, antelopes, bears, and mastodons in grass- ::::> 0' PLIOCENE lands and swamps east of Cascade Range. Oaks, maples, willows in Sandy River valley and rhe Dalles area. 12- Sea shell animals, fish, whales, sea lions in coastal bays. Horses ( Merychippus ) , camels, Creodonts, rodents in John u MIOCENE Day valley. � 0 Forests of Metasequoia, ginkgo, sycamore, oak, and sweet N 0 gum in eastern and western Oregon. z: LU u 26- Abundant and varied shell animals in warm seas occupying Willamette Valley. >- "" OLIGOCENE Three-toed horses, camels, giant pigs, saber-tooth cats, Creodonts, tapirs, rhinos in centra Oregon. ;:;>-- 1 Forests of Metasequoia, ginkgo, sycamore, Katsura. LU"" >-- 37- Tiny four-toed horses, rhinos, tapirs, crocodiles, and Brontotherium in central Oregon.
    [Show full text]
  • Mineralogy of Eocene Fossil Wood from the “Blue Forest” Locality, Southwestern Wyoming, United States
    Article Mineralogy of Eocene Fossil Wood from the “Blue Forest” Locality, Southwestern Wyoming, United States George E. Mustoe 1,*, Mike Viney 2 and Jim Mills 3 1 Geology Department, Western Washington University, Bellingham, WA 98225, USA 2 College of Natural Sciences Education and Outreach Center, Colorado State University, Fort Collins, CO 80523, USA; [email protected] 3 Mills Geological, 4520 Coyote Creek Lane, Creston, CA 93432, USA; [email protected] * Correspondence: [email protected] Received: 7 December 2018; Accepted: 7 January 2019; Published: 10 January 2019 Abstract: Central Wyoming, USA, was the site of ancient Lake Gosiute during the Early Eocene. Lake Gosiute was a large body of water surrounded by subtropical forest, the lake being part of a lacustrine complex that occupied the Green River Basin. Lake level rises episodically drowned the adjacent forests, causing standing trees and fallen branches to become growth sites for algae and cyanobacteria, which encased submerged wood with thick calcareous stromatolitic coatings. The subsequent regression resulted in a desiccation of the wood, causing volume reduction, radial fractures, and localized decay. The subsequent burial of the wood in silty sediment led to a silicification of the cellular tissue. Later, chalcedony was deposited in larger spaces, as well as in the interstitial areas of the calcareous coatings. The final stage of mineralization was the precipitation of crystalline calcite in spaces that had previously remained unmineralized. The result of this multi-stage mineralization is fossil wood with striking beauty and a complex geologic origin. Keywords: fossil wood; Blue Forest; Eden Valley; Lake Gosiute; chalcedony; quartz; calcite; stromatolite; Green River Basin; Wyoming 1.
    [Show full text]
  • Monocot Fossils Suitable for Molecular Dating Analyses
    bs_bs_banner Botanical Journal of the Linnean Society, 2015, 178, 346–374. With 1 figure INVITED REVIEW Monocot fossils suitable for molecular dating analyses WILLIAM J. D. ILES1,2*, SELENA Y. SMITH3, MARIA A. GANDOLFO4 and SEAN W. GRAHAM1 1Department of Botany, University of British Columbia, 3529-6270 University Blvd, Vancouver, BC, Canada V6T 1Z4 2University and Jepson Herbaria, University of California, Berkeley, 3101 Valley Life Sciences Bldg, Berkeley, CA 94720-3070, USA 3Department of Earth & Environmental Sciences and Museum of Paleontology, University of Michigan, 2534 CC Little Bldg, 1100 North University Ave., Ann Arbor, MI 48109-1005, USA 4LH Bailey Hortorium, Plant Biology Section, School of Integrative Plant Science, Cornell University, 410 Mann Library Bldg, Ithaca, NY 14853, USA Received 6 June 2014; revised 3 October 2014; accepted for publication 7 October 2014 Recent re-examinations and new fossil findings have added significantly to the data available for evaluating the evolutionary history of the monocotyledons. Integrating data from the monocot fossil record with molecular dating techniques has the potential to help us to understand better the timing of important evolutionary events and patterns of diversification and extinction in this major and ancient clade of flowering plants. In general, the oldest well-placed fossils are used to constrain the age of nodes in molecular dating analyses. However, substantial error can be introduced if calibration fossils are not carefully evaluated and selected. Here we propose a set of 34 fossils representing 19 families and eight orders for calibrating the ages of major monocot clades. We selected these fossils because they can be placed in particular clades with confidence and they come from well-dated stratigraphic sequences.
    [Show full text]
  • Fossil Palms
    PRINCIPES IVol. lI FossilPalms JosepnA. Ture, M. D. Living palms are familiar plants to oryas (4, p. 172) mentionsthat the dis- "one all who grow them and are a character- covery was of the most significant istic feature of many parts of the trop- finds in recent times" although with in- ics. That palms have a long history in complete evidence it should be classi- time is not always recognized.It is the fied only as palm-like. Ladd and Brown object of this article to illustrate some also illustrated in color the cross-sec- o{ the fossil palms found in the United tion of a fossil palm trunk of a later States, correlating structure of stems, era found on Antigua in the West roots, and leaves with those seen in Indies. It has a light yellow-brown color living palms, the anatomy of which has similar to much of the fossil palm wood beenreviewed and evaluatedby Tomlin- found in Southern California. son in his volume on Palmae in Anato- Arnold (7, p. 341) placesmost of the my of the Monocotyledons(L). fossil palms in North America along Palms first definitely appearedin the with rocks of the Eocene epoch (36'58 Upper Cretaceous rocks, some 63-90 million years ago). There was a shi{t' million years ago by the geologic time ing or migration of palms southward scaleof Kulp (2). A fossil which has due to climatic changes at the end of been called Palmoxylon clillwoodensis the Eocene which continued into the dating from that period has been found Pliocene(I-13 million yearsago).
    [Show full text]
  • Pdf (972.51 K)
    33 Egypt. J. Bot. Vol. 60, No.2, pp. 477-486 (2020) Egyptian Journal of Botany http://ejbo.journals.ekb.eg/ Egyptian Fossil Angiosperm Wood: A Guide to their Anatomical Identification Zainab M. El-Noamani El-Saadawi Lab., Botany Department, Faculty of Science, Ain Shams University, Cairo, 11566, Egypt. FEW of the existing publications on Egyptian fossil plants provide special aids to A identifying fossil wood remains. Two dichotomous keys to the angiosperm petrified wood species reported to date from the Egyptian strata are presented here to facilitate the tentative identification of angiosperm fossil wood specimens. The first key includes 19 species of Palmoxylon which is the morphogenus for the petrified palm stem that is the common representative of monocotyledones (Arecaceae) in the Egyptian fossil flora and can be identified to the species level. The second key contains 46 species of dicotyledonous petrified wood of different families reported in the literature from different ages and locations in Egypt. These keys would benefit palaeobotanists who might find the literature on Egyptian fossil wood not easily accessible. Keywords: Angiosperm, Dichotomous key, Egypt, Fossil wood, Wood anatomy. Introduction by Boureau et al. (1983) from an unknown early Miocene locality in the Western desert without any Identification of fossil wood to the species level description or illustrations is also omitted. has always been a difficult task as compared to modern wood. This is attributable foremost to Material and Methods the preservation state of fossil wood specimens as some specimens may not be in a sufficiently Data in keys I and II are based on descriptions good condition to show important features.
    [Show full text]
  • A Petrified Livistona-Like Palm Stem, Palmoxylon Livistonoides Sp. Nov
    rhe Palaeobotalltsf, 26(3): 197-306, 1980. A PETRIFIED LIVISTONA-LIKE PALM STEM, PALMOXYLON LIVISTONOIDES SP. NOV. FROM THE DECCAN INTERTRAPPEAN BEDS OF INDIA U. PRAKASH & K. AMBWANI Birbal Sahni Institute of Palaeobotany, Lucknow-226 007, India ABSTRACT Palmoxyloll livis/ol/oides sp. nov., a fossil IHlm stem showing close affinities with the extant genus Liris/olla is described here from the Deccan Intertrappean beds of Nawargaon in Wardha District, Maharashtra. Key-words - Petrified palm stem, Palmoxylol/, Eocene, Deccan Interlrappean beds (India). ~m ~n:if ~ 'f~ at~~"\qT~Bnit f~f"WOfT-<i~~ ~ 'fiT~ iiHirTlJ;ififOfT-1fTlf'ff~ f~~ro:g<i 01'0 ;jfTo-;ffl11 wmr t!;'l' 'P1IT ~ eM ~, ~ it ~ ifi ~ ~!ft ~1 « ~ om «<fIfR sr;;rrfcr f~f;;wOfT« ~f.r;o e"lICll11Cl I WWCf 'liB <rnrr ~ 'f>T t!;~ ~~ CRT, lfllfTf<rn~Of f~'fw.rr~f:g<i Of ° "IT ° ~T qfUrcr f.fillT iflIT ~ I INTRODUCTION from a neighbouring village Maragour, whereas Palmoxylon intertrappeum Sahni (1964) is known from Sindhi Vihira. ANEWdescl ibedspecieshereofinpetrifieddetail. Thepalmspecimenstem is Recently, a fossil palm leaf axis, Palmocaulon was collected by one of uS (K.A.) costapalmatum, has been described by from the Deccan Intertrappean beds of Kulkarni and Patil (l977b) from Maragsur. Nawargaon Village (21°1'N: 78°35'E) in Palmoxylon livistonoides resembling the ex• Wardha District, Maharashtra. The palm tant wood of Livistona forms an important wood is very well-preserved and shows a contribution to our knowledge of the Deccan lacunar ground tissue towards the centre. Intertrappean flora of Wardha District. It possesses cortical, dermal and subdermal regions together with the roots attached to it indicating a basal region of the stem.
    [Show full text]