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Science
Olympiad
Division
(Phylum) Pteridospermatophyta |
Seed
ferns (Pteridospermatophyta) range from the Devonian to the Cretaceous. They flourished from the Carboniferous to the Permian. Pteridosperms had fern-like foliage,
but reproduced with seeds (Selmeier, 1996, p. 142). Seed
ferns exhibited both vine-like and arborescent forms. The
term pteridosperm ("seed fern") is descriptive but, misleading
as these plants are really early gymnosperms (Cleal & Thomas,
2009, p. 139). Seed ferns actually represent several distinct gymnosperm groups.
Seed Fern Characteristics
Without the knowledge of reproductive structures the foliage
of seed ferns is difficult to distinguish from ferns. Fronds
are pinnately divided as in the ferns. However, fertile
fronds possess pollen organs or ovules instead of spore
producing
structures. Fern spores are wind dispersed. Medullosans
pollen grains, at 0.3 mm in diameter, were five times larger
than
average.
This
has
led some
paleontologists
to suspect that medullosans were pollinated by insects
(Kenrick & Davis, 2004, p. 93). Seeds were grouped on special
branches or positioned on leaves along the midrib or margins.
The trunks of many seed ferns consisted of separate vascular
segments in the form of wedges (polystele). In some species
the wedges produced
secondary xylem (wood) only to the inside,
others produced wood towards the inside and outside,
still others produced wood all the way around the wedge.
There is a distinct evolutionary trend in the number of
vascular
bundles embedded in the pith along with the position of
peripheral vascular bundles. Over time, a single, deeply
divided vascular
bundle evolved into three or more. Outer vascular bundles
became fused, forming rings of secondary
wood by the Lower Permian (Jung, 1996, p. 158). Glossopteris is
a seed fern with a eustele vascular bundle (concentric
vascular
bundles
with enclosed pith), which is characteristic of conifers
and angiosperms. Both the polystele and eustele wood of
seed ferns was composed of conifer-like wood.
Seed Fern Trees
Among the arborescent seed ferns Medullosa was
the largest at 10m (Willis & McElwain, 2002, p. 112). Medullosa had
a crown of large fronds. Fronds were enormous reaching
a length
of
7
meters.
Fronds
were pinnately
divided, dichotomously branched, and spirally arranged
around the stem. The trunk was composed of vascular segments.
Secondary
xylem formed towards the inside of primary xylem (opposite
of living plants). The secondary xylem was surrounded by
the vascular cambium, secondary
phloem,
and cortical tissues. The external part of the lower trunk
was clothed in large prop roots. Medullosa seemed
to prefer mineral rich soils to peaty substrates. Medullosa lived
in fire prone parts of the mire where its resin rich wood
and abundance of foliage acted as a good source of fuel
(Kenrick & Davis, 2004, p. 93).
Neuropteris and Alethopteris are
common seed fern fronds. Whittleseya, Dolerotheca,
and
Aulacotheca are pollen blossoms. Trigonocarpus is
the cast of large pteridosperm seeds. Pachytesta is
the permineralized form of these seeds. Myeloxylon is
the frond base of Medullosa and
is often found attached to the exterior of the lower trunk
(Jung, 1996, p. 158).
Science Olmpiad Fossil Event
The 2016 Science Olympiad Fossil List includes the genus
Glossopteris within the phylum Pteridospermatophyta (Seed Ferns).
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Seed
Fern
Neuropteris dussarti
Upper Carboniferous, Westfalien
Piesberg/Osnabruck, Germany
Plate 8 cm x 7 cm
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Seed Fern
Neuropteris attenuata
Upper Carboniferous, Westfalien
Piesberg/Osnabruck, Germany
Plate 12 cm x 7.5 cm |
Seed
Fern
Neuropteris scheuchzeri
Upper Carboniferous, Westfalien
Piesberg/Osnabruck, Germany
Plate 7.5 cm x 7.3 cm |
Seed
Fern
Alethopteris davreuxi
Upper Carboniferous, Westfalien
Piesberg/Osnabruck, Germany
Plate 8.8 cm x 6.2 cm |
Seeds from Seed Fern in Bituminous Coal
Trigonocarpus sp.
Collected in Maryland/Pennsylvania Area
5 to 6 cm in length
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Fern (Neuropterid Group)
Cyclopteris trichomanoides
Mazon Creek, Illinois
Carbondale Formation, Francis Creek Shale Member
Paleozoic; Pennsylvanian
9.5 cm long x 7 cm wide
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Seed Fern
Rhexoxylon sp.
Gowke, Zimbabwe
Triassic
20.5 cm x 17 cm |
Seed Fern
Pentoxylon-like specimen
Queensland, Australia
20.5 cm x 15 cm |
Seed Fern
Glossopteris sp.
Moranbah, Queensland, Australia
Permian
3.5 cm diameter x 1.4 cm tall |
Seed Fern
Glossopteris Leaf & Seed Scale
Glossopteris sp. &
Squamella australis
Mudgee, New South Wales, Australia
Permian
Plate 9.5 cm x 6 cm
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Glossopteris Leaves
Upper
Permian
Illawarra Coal Measures
Dunedoo, New South Wales, Australia
6 cm x 11 cm
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Bibliography
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Cleal
C.J. & Thomas, B.A. (2009). Introduction to Plant
Fossils. United
Kingdom: Cambridge University Press.
Jung,
W. (1996). Ferns, Cycads, or What? In Dernbach, U. Petrified
Forest: The World's 31 Most Beautiful Petrified Forests (pp.
155-159). Germany:
D’ORO Publishers.
Kenrick,
P. and Davis, P. (2004). Fossil Plants. Smithsonian
Books: Washington.
Selmeier,
A. (1996). Identification of Petrified Wood Made Easy.
In Dernbach, U. Petrified Forest: The World's 31
Most Beautiful Petrified Forests (pp. 136-147). Germany:
D’ORO Publishers.
Willis,
K.J. & McElwain, J.C. (2002). The Evolution of
Plants. New York: Oxford University Press. |
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