New insights into Mesozoic cycad evolution: an exploration of anatomically preserved Cycadaceae seeds from the Jurassic Oxford Clay biota

Alan R.T. Spencer, Russell Garwood, Andrew R. Rees, Robert J. Raine, Gar W. Rothwell, Neville T.J. Hollingworth, Jason Hilton

    Research output: Contribution to journalArticlepeer-review

    Abstract


    Most knowledge concerning Mesozoic Era floras has come from compression fossils. This has been augmented in the last 20 years by rarer permineralized material showing cellular preservation. Here, we describe a new genus of anatomically preserved gymnosperm seed from the Callovian–Oxfordian (Jurassic) Oxford Clay Formation (UK), using a combination of traditional sectioning and synchrotron radiation X-ray micro-tomography (SRXMT). Oxfordiana motturii gen. et sp. nov. is large and bilaterally symmetrical. It has prominent external ribs, and has a three-layered integument comprising: a narrow outer layer of thick walled cells; a thick middle parenchymatous layer; and innermost a thin fleshy layer. The integument has a longitudinal interior groove and micropyle, enveloping a nucellus with a small pollen chamber. The large size, bilateral symmetry and integumentary groove demonstrate an affinity for the new species within the cycads. Moreover, the internal groove in extant taxa is an autapomorphy of the genus Cycas, where it facilitates seed germination. Based upon the unique seed germination mechanism shared with living species of the Cycadaceae, we conclude that O. motturii is a member of the stem-group lineage leading to Cycas after the Jurassic divergence of the Cycadaceae from other extant cycads. SRXMT—for the first time successfully applied to fossils already prepared as slides—reveals the distribution of different mineral phases within the fossil, and allows us to evaluate the taphonomy of Oxfordiana. An early pyrite phase replicates the external surfaces of individual cells, a later carbonate component infilling void spaces. The resulting taphonomic model suggests that the relatively small size of the fossils was key to their exceptional preservation, concentrating sulfate-reducing bacteria in a locally closed microenvironment and thus facilitating soft-tissue permineralization.
    Original languageEnglish
    JournalPeerJ
    Early online date28 Aug 2017
    DOIs
    Publication statusPublished - 2017

    Keywords

    • Palaeobotany
    • Fossil
    • Cycad
    • Cycadeospermum
    • Cycas
    • Oxford Clay Formation
    • Taphonomy
    • Gymnosperm
    • Ovule
    • 3D Reconstruction

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    • ICAL: Interdisciplinary Centre for Ancient Life

      Garwood, R. (PI), Wogelius, R. (PI), Sansom, R. (CoI), Buckley, M. (CoI), Chamberlain, A. (CoI), Manning, P. (CoI), Egerton, V. (CoI), Sellers, W. (CoI), Nudds, J. (CoI), Bulot, L. G. (CoI), Brocklehurst, R. (PGR student), Brassey, C. A. (CoI), Keating, J. (CoI), La Porta, A. (CoI), Brocklehurst, R. (PGR student), Callender-Crowe, L. (PGR student), Wallace, E. (PGR student), Chester, J. (PGR student), Davenport, J. (PGR student), Tuley, K. (PGR student), Lomax, D. (Researcher), Reeves, J. (PGR student), Smart, C. (PGR student), Ferro, C. (PGR student), Karoullas, C. (PGR student), Heath, J. (PGR student), Dickson, A. (PGR student), Austin Sydes, L. (PGR student), McLean, C. (PGR student), Harvey, V. (PGR student) & Jones, K. (PI)

      Project: Research

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