Untersuchungen über fossile Platanenhölzer Beiträge zu einer Monographie der Gattung <i>Platanoxylon</i> ANDREǍNSZKY

Süß, H.; Müller‐Stoll, Wolfgang R.

doi:10.1002/fedr.19770880102

Cited by 18 publications

(8 citation statements)

References 21 publications

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“…Of the body fossils originally Hendel (1931Hendel ( -1936 .NA Not an agromyzid in modern sense (Hendel, 1931(Hendel, -1936 von Heyden (1862), Sittig (1927) .U Apparently identical to mine described by Berger (1949;see Stoll (1975Stoll ( , 1977 .A ''Pith flecks'' in wood, analogous to Phytobia traces.…”

mentioning

confidence: 96%

Distinguishing Agromyzidae (Diptera) Leaf Mines in the Fossil Record: New Taxa from the Paleogene of North America and Germany and Their Evolutionary Implications

et al. 2010

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Fossilized leaf mines and other traces of phytophagous insects provide a unique window into ecological and evolutionary associations of the past. Leaf-mining flies (Diptera: Agromyzidae) are an important component of the recent leaf-mining fauna, but their fossil record is sparse compared to other mining insect lineages; many putative agromyzid body fossils and traces are dubiously assigned. Agromyzid leaf mines often can be distinguished from those of other insects by the presence of an intermittent, fluidized frass trail that may alternate between the sides of the mine. Here, we describe two new Paleogene leaf mine fossils, Phytomyzites biliapchaensis Winkler, Labandeira and Wilf n. sp. from the early Paleocene of southeastern Montana, USA, occurring in leaves of Platanus raynoldsii (Platanaceae); and Phytomyzites schaarschmidti Wappler n. sp., from the middle Eocene of Messel, Germany, occurring in leaves of Toddalia ovata (Rutaceae). These fossils both exhibit frass trails indicative of an agromyzid origin, and P. biliapchaensis also exhibits associated stereotypical marks identical to damage caused by feeding punctures of extant adult female Agromyzidae prior to oviposition. Phytomyzites biliapchaensis represents the earliest confirmed record of Agromyzidae, and one of the earliest records for the large dipteran clade Schizophora. Plant hosts of both species belong to genera that are no longer hosts of leaf-mining Agromyzidae, suggesting a complex and dynamic history of early host-plant associations and, for the early Paleocene example, an evolutionary, possibly opportunistic colonization in the midst of the ecological chaos following the end-Cretaceous event in North America.

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confidence: 96%

Distinguishing Agromyzidae (Diptera) Leaf Mines in the Fossil Record: New Taxa from the Paleogene of North America and Germany and Their Evolutionary Implications

et al. 2010

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“…50), we have not observed any simple perforation plates in our samples of platanoid wood. Secondly, as Süss & Müller-Stoll (1977) described, some platanoid woods have spiral thickening in the vessel elements. This feature is unknown among extant Platanus woods (Wheeler & Manchester 2002).…”

Section: Dryoxylon Schleiden In Schmidmentioning

confidence: 75%

Fossil angiosperm wood and its host deposits from the periphery of a dominantly effusive ancient volcano (Doupovské hory Volcanic Complex, Oligocene-Lower Miocene, Czech Republic): systematics, volcanology, geochronology and taphonomy

Sakala¹,

Rapprich²,

Pécskay³

2010

Bull. Geosci.

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A variety of fossil woods occur on the northern margin of the Doupovské hory Volcanic Complex in the northwestern part of the Czech Republic. The woods were buried by three different processes reflecting three different settings. First, a large area between the towns of Kadaň and Klášterec is covered by an up to 100 m thick sequence of lahar and debris avalanche deposits. These flows and avalanches gathered wood of Liriodendron, Lauraceae, Platanus, Cercidiphyllum, ?Craigia and Styracaceae from both the volcanic complex slopes and adjacent plains. Second, a rich assemblage of fossil woods with thermophilous elements such as Lauraceae and palms was preserved on the northern volcanic complex periphery by a Strombolian eruption of a monogenic cone. Third, a shallow lake formed to the side of the volcanic complex, where Platanus trunks were fossilized in the travertine. The wood of Liriodendron has never been previously recorded in the localities representing volcanic complex foothills, but is common in the local lahar deposits. This distribution leads us to hypothesize that Liriodendron forests dominated higher topographic levels of the Doupovské hory Volcanic Complex, reaching, but probably not exceeding 1000 m a.s.l.

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“…Some years later, Süss and Müller-Stoll (1977) consider Plataninium an inutile, ambiguous name that has to be invalidated. Therefore, this name was several times subject of revision or dispute, some species being redescribed as belonging to other genera, for exemple: Plataninium subaffine Vater, 1884, that became Hedycaryoxylon subaffine (Vater) Süss, 1960; or Plataninium aceroides (Goeppert) Windisch, 1886, that became Fagoxylon acerinum (Windisch) Süss, 1986; or have been replaced by names as Platanus, Platanoxylon or Spiroplatanoxylon (see Edwards and Jogmans, 1931;Süss, 1960Süss, , 1971Süss, , 1986Süss, , 2007Süss and Müller-Stoll, 1977). The name Plataninium is still used by some American, Asian and even European scientists, and considered as a primitive type.…”

Section: Affinities and Discussionmentioning

confidence: 99%

“…ogasawarae Takahashi et Suzuki, 2003, described from Cretaceus of Japan. The morphogenus Platanoxylon Andreánszky, 1951(ex Prakash et al 1971 was also subject of revision and dispute, at least in the last time (Süss & Müller-Stoll, 1977;Süss, 2007, with references). After all these, a clear diagnosis has to separate the three admitted genera of fossil plants.…”

Section: Affinities and Discussionmentioning

confidence: 99%

“…Hence, after the revision of Süss (2007), some already described species were assigned to this morphogenus (Selmeier, 1996 considered it as organ-genus!) as it follows: -Plataninium haydenii Felix, 1894, P. pacificum Platen, 1908and P. crystallophilum Platen, 1908 were revised to Platanoxylon haydenii (Felix) Süss et Müller-Stoll, 1977, Platanoxylon pacificum (Platen) Süss et Müller-Stoll, 1977, and respectively to Platanoxylon crystallo-philum (Platen) Süss et Müller-Stoll, 1977. -Moreover, six species were validated by Süss et Müller-Stoll (1977) as correctly attributed to Platanoxylon: P. andreanszkyi Süss et Müller-Stoll, 1977, P. hungaricum Süss et Müller-Stoll, 1977, P. palibacsii Süss et Müller-Stoll, 1977, P. sarmaticum Süss et Müller-Stoll, 1977, P. catenatum Süss et Müller-Stoll, 1977, also described by us in the South Apuseni Mountains , and P. cohenii (Schuster) Süss, 1980, adding other generic identification as Platanoxylon sp., described from Hungary, Czech Republic and Germany by Andreánszky (1952), as belonging to Platanoxylon, according to Selmeier (1996Selmeier ( , 2001 and Gottwald (2000). Also, the specimen described by Petrescu & Vasiliu (1987) from Romania is a Platanoxylon.…”

Section: Affinities and Discussionmentioning

confidence: 99%

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Fossil Woods From Bozovici (Sw Romania)

Iamandei¹,

Iamandei²,

Stoia³

2019

Actapalrom

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A palaeoxylotomical study was done on several samples from a private collection of petrified wood found in Bozovici area, which were taxonomically identified. Bozovici area is a small Badenian depression filled by coarse continental deposits, with some interbedded coal and volcanic tuffs. The frequent lateral facies variations and the few fossils of fresh water fauna make difficult a stratigraphic correlation of these deposits. Those samples of fossil wood were identified as remains of Glyptostroboxylon rudolphii Dolezych et Van der Burgh and Spiroplatanoxylon den-siradiatum (Petrescu) Süss and an extended discussion concerning the systematics of these taxa was made. Advanced studies on more numerous samples coming from Bozovici area could contribute to a better palaeoenvironmental and palaeoclimatic reconstruction of that area, during Badenian time.

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Untersuchungen über fossile Platanenhölzer Beiträge zu einer Monographie der Gattung Platanoxylon ANDREǍNSZKY

Cited by 18 publications

References 21 publications

Distinguishing Agromyzidae (Diptera) Leaf Mines in the Fossil Record: New Taxa from the Paleogene of North America and Germany and Their Evolutionary Implications

Distinguishing Agromyzidae (Diptera) Leaf Mines in the Fossil Record: New Taxa from the Paleogene of North America and Germany and Their Evolutionary Implications

Fossil angiosperm wood and its host deposits from the periphery of a dominantly effusive ancient volcano (Doupovské hory Volcanic Complex, Oligocene-Lower Miocene, Czech Republic): systematics, volcanology, geochronology and taphonomy

Fossil Woods From Bozovici (Sw Romania)

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