2016
DOI: 10.14446/fi.2016.131
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Foliage accumulations of Osmunda lignitum (osmundaceae) in the Oligocene of northern Italy and western Germany

Abstract: Accumulations of Osmunda (Plenasium) lignitum (Giebel) Stur fern foliage have been recently recovered in the Oligocene deposits of northern Italy at Cassinelle and western Germany at Niederpleis-1 (Sankt Augustin; Winterscheid 2006). They morphologically match other European records distributed from the Eocene to the Oligocene (– early Miocene). Material from both sites represents sterile pinnae compressions with preserved leaf anatomy. The data obtained on leaf cuticles correspond to most of the previous find… Show more

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(4 citation statements)
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“…Osmunda bromeliifolia from the Miocene of Japan (Endo, 1961), O. to-tangensis (Colani) Guo from the Miocene-Pliocene of Yunnan, China (WGCPC, 1978), and O. lignitum (Giebel) Stur from the Eocene-Miocene of the Northern Hemisphere (Stur, 1870;Miller, 1967Miller, , 1971Huzioka & Takahasi, 1970;Barthel, 1976;Mai & Walther, 1978, 1985; WGCPC, 1978;Guo, 1985;Wilde, 1989;Kvaček & Hably, 1991;Frankenhäuser & Wilde, 1993;Petrescu et al, 1995;Kvaček & Walther, 1998;Wilde & Frankenhäuser, 1998;Kvaček & Martinetto, 2016), share the same characters of dentate and articulate pinnules with our fossils as well as extant species of the subgenus Plenasium. Differences between the present fossil specimens and O. bromeliifolia have been discussed in aforementioned comparisons with the extant species.…”
Section: Comparisons With Fossil Speciesmentioning
confidence: 99%
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“…Osmunda bromeliifolia from the Miocene of Japan (Endo, 1961), O. to-tangensis (Colani) Guo from the Miocene-Pliocene of Yunnan, China (WGCPC, 1978), and O. lignitum (Giebel) Stur from the Eocene-Miocene of the Northern Hemisphere (Stur, 1870;Miller, 1967Miller, , 1971Huzioka & Takahasi, 1970;Barthel, 1976;Mai & Walther, 1978, 1985; WGCPC, 1978;Guo, 1985;Wilde, 1989;Kvaček & Hably, 1991;Frankenhäuser & Wilde, 1993;Petrescu et al, 1995;Kvaček & Walther, 1998;Wilde & Frankenhäuser, 1998;Kvaček & Martinetto, 2016), share the same characters of dentate and articulate pinnules with our fossils as well as extant species of the subgenus Plenasium. Differences between the present fossil specimens and O. bromeliifolia have been discussed in aforementioned comparisons with the extant species.…”
Section: Comparisons With Fossil Speciesmentioning
confidence: 99%
“…During the Paleocene, Osmunda was found in Asia, such as O. greenlandica and O. sachalinensis Kryshtofovich from northeastern China (Tao & Xiong, 1986;Wang et al, 2006) and North America indicated by O. heeri, O. greenlandica, O. macrophylla, O. pluma Miller, O. precinnamomea Miller, and O. arnoldii Miller from the northern, western, and northwestern North America (Brown, 1962;Miller, 1967Miller, , 1971Zhang et al, 1980). In the Eocene, the genus was scattered in Europe, Asia, and North America, indicated by O. lignitum from the Eocene of Europe and East Asia (Matsuo, 1963(Matsuo, , 1967Tanai, 1970;Barthel, 1976;Mai & Walther, 1978, 1985Guo, 1985;Wilde, 1989;Kvaček & Hably, 1991;Frankenhäuser & Wilde, 1993;Petrescu et al, 1995;Kvaček & Walther, 1998;Wilde & Frankenhäuser, 1998;Kvaček & Martinetto, 2016), O. dowkeri (Carruthers) Chandler from the Eocene of Europe and North America (Kidston & Gwynne-Vaughan, 1914;Arnold, 1952;Chandler, 1965;Miller, 1967Miller, , 1971). In the Oligocene, fossil records of the genus occurred in Europe and Asia, including O. lignitum from Germany (Kvaček & Martinetto, 2016), O. sachalinensis and O. japonica Thunb.…”
Section: Biogeographic Implicationsmentioning
confidence: 99%
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