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UNIVERSITY MÜNSTER |
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All modern clubmosses or lycopods are small herbaceous
plants. Most of their late Palaeozoic, particularly their Carboniferous
relatives were large trees. Several genera are known. One of
the best known tree-like lycopods is Lepidodendron. Sigillaria
is another example of a lycopod tree. Genera are distinguished on
the basis of the shape of the leaf cushions on the stems, their anatomy,
their reproductive structures and their growth habit. During most
of the Westphalian arborescent lycopods were the dominant elements in coal
swamp floras and hence also the most important biomass producers.
Up to 80% of the North American and European Westphalian coals
can consist of biomass derived from arborescent lycopods. Tree-like
lycopods were heterosporous; in some forms the megaspores with surrounding
megasporangia and megasporophylls look almost seed-like.
Unlike in any other type of tree which all have secondary
growth concentrated in the xylem (wood), the secondary growth of arborescent
lycopods mainly took place in the cortex (bark). Several examples of in
situ preserved fossil lycopod forest are known. Most arborescent
lycopods became extinct by the end of the Westphalian. Apart from arborescent
forms also herbaceous lycopods are known. These include homosporous
forms similar to most modern lycopods and heterosporous forms similar to
the modern Selaginella. Some authors even assign Carboniferous forms
to the extant genus Selaginella. If this would be true, this would
be the longest living genus of higher land plants.
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| Lycophytes | Virtual Paleobotany Laboratory | links to pictures and further info |
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| Large in situ lycopod trunk | Astrobiology UCLA | cover of Geotimes |
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| One of the most common and most widespread Carboniferous tree lycopods is Lepidodendron. The genus was orginally described for stem surfaces showing the characteristic spirally arranged diamond-shaped, vertically positioned leaf cushions. Some Lepidodendron species could be up to ca. 40 m high. Most peculiar is their anatomy showing that the secondary growth mainly took place in the cortex; the proportion of xylem (wood) is relatively small. During their life the trees shed parts of their outer bark and basal parts of the trunks and larges stems typically show various stages of decortication. Lepidodendron trees rooted horizontally, indicating humid environments. Root systems are known as Stigmaria. Several types of branching patterns of aerial stems have been distinguished, on the basis of which the genus has been differentiated into several genera. Branching can be lateral or dichotomous; large branch scars of lateral branches have been described as Ulodendron. Leaves were long, narrow and stiff (Lepidophyllum); those of the the ultimate branches being smaller and needle-like. The plants were heterosporous and some of the strobili, known as Lepidostrobus, could reach a length of nearly 1 m. Isolated sporophylls are known as Lepidostrobophyllum. Lepidondendron became almost completely extinct by the end of the Westphalian. | ||||
| Lepidodendron | Hans' (Steur) Paleobotany Page | reconstruction with different organs |
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| Lepidodendron | ||||
| Lepidodendron aculeatum | M. Hieb's Plant Fossils of W. Virginia | figured upside down |
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| Lepidodendron aculeatum | Geol.-Paläontol. Mus., Univ. Münster |
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| Lepidodendron aculeatum | Fossils of Nova Scotia |
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| Lepidodendron obovatum | Museum of Natural History, Sendai | German material in Japan ! |
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| Lepidodendron obovatum | M. Hieb's Plant Fossils of W. Virginia |
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| Lepidodendron aculeatum | M. Hieb's Plant Fossils of W. Virginia | |||
| Lepidodendron aculeatum | M. Hieb's Plant Fossils of W. Virginia | |||
| Lepidodendron worthenii | M. Hieb's Plant Fossils of W. Virginia |
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| Lepidodendron | Fossils of Nova Scotia |
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| Lepidodendron | Fossils of Nova Scotia |
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| Lepidodendron | Fossils of Nova Scotia | foliated branches |
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| Lepidodendron | Fossils of Nova Scotia |
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| Lepidodendron | Fossils of Nova Scotia |
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| Lepidodendron | Fossils of Nova Scotia | decorticated axis |
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| Lepidodendron | Ohio History Central |
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| Lepidodendron | M. Hieb's Plant Fossils of W. Virginia |
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| Lepidodendron | M. Hieb's Plant Fossils of W. Virginia | ultimate branches |
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| Lepidodendron | M. Hieb's Plant Fossils of W. Virginia | Ulodendron aspect |
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M. Hieb's Plant Fossils of W. Virginia | Ulodendron aspect |
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| Lepidodendron | Mazon Creek Exhibit, Illinois State Mus. |
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| Lepidodendron | M. Hieb's Plant Fossils of W. Virginia | branching |
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| Lepidodendron | Collection Jens-Wilhelm Janzen |
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| Lepidodendron | Musée de fossiles, Montceau-les-Mines | stem surface and ultimate branches |
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| Lepidodendron | Dept. Botany, Hawai | also modern lycopods |
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| Lepidodendron and Stigmaria | R.A. Spicer, Open Univ., Milton Keynes |
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| Lepidodendron | K. Pigg's "Plant Fossils and Evolution" |
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| Lepidodendron | K. Pigg's "Plant Fossils and Evolution" | cross section of a stem |
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| Lepidodendron | Bot. Soc. America, Online Image Coll. | cross section, small stem |
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| Lepidodendron | Bot. Soc. America, Online Image Coll. | as above, high resolution |
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| Lepidodendron selaginelloides | Bot. Soc. America, Online Image Coll. | coal ball; leaf base with ligule |
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| Lepidodendron selaginelloides | Bot. Soc. America, Online Image Coll. | as above, high resolution |
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| Lepidodendron | Bot. Soc. America, Online Image Coll. | coal ball: cross section |
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| Lepidodendron | Bot. Soc. America, Online Image Coll. | as above, high resolution |
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| Lepidodendron | Fossil plants, N. Anthracite Coal Field |
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| Lepidodendron | Virtual Paleobotany Laboratory |
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| Halonia (Lepidodendron) | M. Hieb's Plant Fossils of W. Virginia |
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| Lepidophyllum (this genus is also known as Cyperites or Lepidophylloides) | ||||
| Lepidodendron sp. | M. Hieb's Plant Fossils of W. Virginia | a magnificent branching axis ! |
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| Lepidophyllum sp. | M. Hieb's Plant Fossils of W. Virginia | small foliated axes | ||
| Lepidophyllum sp. | M. Hieb's Plant Fossils of W. Virginia | as above, one with cones |
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| Lepidophyllum sp. | Mazon Creek Exhibit, Illinois State Mus. |
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| Lepidophylloides | Virtual Paleobotany Laboratory |
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| Lepidophylloides | Virtual Paleobotany Laboratory |
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| Cyperites bicarinatus | Fossil plants, N. Anthracite Coal Field |
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| Lepidostrobus | ||||
| Lepidostrobus sp. | Mazon Creek Exhibit, Illinois State Mus. |
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| Lepidostrobus sp. | M. Hieb's Plant Fossils of W. Virginia |
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| Lepidostrobus sp. | M. Hieb's Plant Fossils of W. Virginia |
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| Lepidostrobus | Collection Jens-Wilhelm Janzen |
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| Lepidostrobus | Fossil plants, N. Anthracite Coal Field |
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| Lepidostrobus | Fossils of Nova Scotia |
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| Lepidostrobus | Fossils of Nova Scotia |
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| Lepidostrobus | Virtual Paleobotany Laboratory | coal ball peel |
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| Lepidostrobus | Virtual Paleobotany Laboratory | coal ball peel |
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| Lepidostrobus sp. | Paläobotanik Münster | anatomically preserved |
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| Lepidostrobophyllum | ||||
| Lepidostrobophyllum sp. | Mazon Creek Exhibit, Illinois State Mus. |
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| Lepidostrobophyllum sp. | M. Hieb's Plant Fossils of W. Virginia |
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| Lepidostrobophyllum lanceolatum | Fossils of Nova Scotia |
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| Lepidostrobophyllum | Virtual Paleobotany Laboratory |
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| Lepidophloios differs from Lepidodendron in having diamond-shaped leaf cushions that wider than high but also spirally arranged. This tree had the same type of rooting and foliage types as Lepidodendron. | ||||
| Lepidophloios laricinus | Fossils of Nova Scotia |
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| Lepidophloios laricinus | Fossils of Nova Scotia |
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| Lepidophloios laricinus | Fossils of Nova Scotia |
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| Lepidophloios | Virtual Paleobotany Laboratory |
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| Lepidophloios sp. | Paläobotanik Münster |
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| Lepidocarpon is a megasporophyll holding a megasporangium with only a single functional megaspore. The megapsporophyll encloses the megasporangium completely thus giving optimal protection. The whole unit (megasporophyll + megasporangium) is shed from the cone. Lepidocarpon thus already pretty much shows a seed-like morphology. | ||||
| Lepidocarpon | Virtual Paleobotany Laboratory |
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| Sigillaria is another very common and widepread lycopod tree. Leaf cushions are rhomboidal in outline and usually placed in distinct vertical rows; in some species rows are separated by ridges. Unlike Lepidodendron, Sigillaria did not branch very often, usually one or two times. Rooting systems and leaves are of the same type as in Lepidodendron. The strobili, known as Sigillariostrobus, were borne directly on the main stem. Most Sigillaria species became extinct by the end of the Westphalian but a few forms survived and persisted into the Permian. | ||||
| Sigillaria | Mus. Natural History, Univ. Michigan | reconstruction of a tree |
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| Sigillaria | M. Hieb's Plant Fossils of W. Virginia | reconstruction of a tree |
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| Sigillaria | ||||
| Sigillaria sp. | M. Hieb's Plant Fossils of W. Virginia | decorticated stem |
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| Sigillaria brardii | Fossil plants, N. Anthracite Coal Field |
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| Sigillaria | Fossil plants, N. Anthracite Coal Field | decorticated axis |
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| Sigillaria | Collection Jens-Wilhelm Janzen |
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| Sigillaria | Virtual Paleobotany Laboratory |
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| Sigillaria | Computational Palaeontology | computer reconstruction |
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| Sigillaria davreuxii | M. Hieb's Plant Fossils of W. Virginia | |||
| Sigillaria davreuxii | M. Hieb's Plant Fossils of W. Virginia |
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| Sigillaria cf. davreuxii | M. Hieb's Plant Fossils of W. Virginia | |||
| Sigillaria scutellata | Fossils of Nova Scotia |
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| Sigillaria elegans | Fossils of Nova Scotia |
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| Sigillaria tessalata | Fossils of Nova Scotia |
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| Sigillaria tessalata | Fossils of Nova Scotia |
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| Syringodendon sp. | M. Hieb's Plant Fossils of W. Virginia | decorticated Sigillaria |
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| Sigillariostrobus | ||||
| Sigillariostrobus sp. | M. Hieb's Plant Fossils of West Virginia |
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| Stigmaria is the rooting system of tree lycopods, Lepidodendron, Lepidophloios and Sigillaria. The woody, a few times bifurcating axes borne hollow tube-like appendages which had the function of roots. Such rooting systems are called rhizomorphic; Isoetes is one of the very few modern lycopods with a rhizomorphic rooting system. Stigmaria rootlet beds are very common and often occur underneath coal seams. Most famous are in situ preserved forest stands with several stigmarian tree trunks, e.g. the Fossil Grove in Glasgow (Scotland) and Joggings (Nova Scotia). | ||||
| Stigmaria ficoides | M. Hieb's Plant Fossils of W. Virginia |
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| Stigmaria ficoides | M. Hieb's Plant Fossils of W. Virginia | |||
| Stigmaria ficoides | Fossils of Nova Scotia |
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| Stigmaria ficoides | Fossils of Nova Scotia |
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| Stigmaria ficoides | Fossils of Nova Scotia |
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| Stigmaria ficoides | Fossils of Nova Scotia |
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| Stigmaria sp. | Fossils of Nova Scotia |
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| Stigmaria | Bot. Soc. America, Online Image Collection | cross section |
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| Stigmaria | Bot. Soc. America, Online Image Collection | as above, high resolution |
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| Stigmaria | Ohio History Central |
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| Stigmaria | Virtual Paleobotany Laboratory |
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| Stigmaria | Virtual Paleobotany Laboratory |
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| Stigmaria | Virtual Paleobotany Laboratory | anatomically preserved |
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| Stigmaria | Museum am Schölerberg, Osnabrück | very large specimen |
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| Several examples of fossil lycopod forests are known. These forests consist of upright standing tree stumps, i.e. the rooting system and the lower portion of the stem. The Fossil Grove in Glasgow (Scotland) and Joggins (Nova Scotia) are among the most famous. | ||||
| The Fossil Grove | Hunterian Museum Glasgow |
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| The Fossil Grove | Astrobiology UCLA | in 1887 |
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| The Fossil Grove | Astrobiology UCLA |
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| Joggins |
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| Chaloneria is was an up to 2 m high unbranched heterosporous lycopod with axes up to 10 cm in diameter with roots of the Stigmaria-Isoetes type. The microspores are of the Endosporites type, whereas the megaspores are of the Valvisisporites type. This taxon is known from North American coals balls. | ||||
| Chaloneria | Kathleen Pigg's "Plant Fossils and Evolution" | longitudinal section through the base |
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| Chaloneria | Kathleen Pigg's "Plant Fossils and Evolution" | cross section |
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| Chaloneria | Kathleen Pigg's "Plant Fossils and Evolution" | bark and outer stem surface |
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| Chaloneria | Kathleen Pigg's "Plant Fossils and Evolution" | phloem |
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| Chaloneria | Kathleen Pigg's "Plant Fossils and Evolution" | fertile and vegetative stems |
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| Endosporites | Kathleen Pigg's "Plant Fossils and Evolution" | microspores of Chaloneria |
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| Valvisisporites | Kathleen Pigg's "Plant Fossils and Evolution" | megaspore of Chaloneria |
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| Chaloneria | Kathleen Pigg's "Plant Fossils and Evolution" | megagametophyte |
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| Chaloneria | Kathleen Pigg's "Plant Fossils and Evolution" | megagametophyte |
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| Chaloneria | Kathleen Pigg's "Plant Fossils and Evolution" | megagametophyte |
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| Chaloneria | Kathleen Pigg's "Plant Fossils and Evolution" | megagametophyte |
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| Lycopodites is a genus for small, herbaceous lycopods | ||||
| Lycopodites | Kathleen Pigg's "Plant Fossils and Evolution" |
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| Lycopod megaspores | ||||
| Thomasonia | Bot. Soc. America, Online Image Collection |
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| Thomasonia | Bot. Soc. America, Online Image Collection | as above, high resolution |
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| Minerisporites mirabilis | Bot. Soc. America, Online Image Collection |
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| Minerisporites mirabilis | Bot. Soc. America, Online Image Collection | as above, high resolution |
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| Molaspora lobata | Bot. Soc. America, Online Image Collection |
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| Molaspora lobata | Bot. Soc. America, Online Image Collection | as above, high resolution |
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| Megaspore of Lepidodendron | Virtual Paleobotany Laboratory |
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| Some information on modern lycopods | ||||
| Modern lycopods | Univ. California Mus. Paleontology, Berkeley |
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This page was launched October 1999; last modifications
and updates are from January 2002. The links give the most
direct connections to pictures available on the web; in many cases they
are from sites that have additional palaeobotanical information.
The above ratings refer to:
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| © Forschungsstelle für Paläobotanik, Westfälische Wilhelms-Universität Münster |
updated: January 2002
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