Beautiful rare Lepidodendron cone fossil plant in Mazon Creek like nodule half

Description

My genuine specimens will be delivered with a "Certificate of authenticity, age and origin"  and scientific papers allowing plant identification !
I combine shipping costs.
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I will send You a combine invoice.
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Specimen:
Lepidostrobus variabilis
Lidney & Hutton
- arborescent, 310 Mya  old, Club Moss (Lepidodendron) cone
Locality:
All detailed and accurate data will be provided with the specimen
Stratigraphy:
Upper Carboniferous –
Pennsylvanian,
Bashkirian
,
Westphalian A
Age:
ca. 314 Mya
Matrix size:        ca. 4,8 x 2,5 x 1,0 cm ( white square is 1,0 x 1,0 cm)
Description:
Nice
specimen of Lepidodendron cone
Lepidostrobus variabilis
Lidney&  Hutton
- cone preserved in Mazon Creek like siderite nodule half from Europe - Old Collection. Today this is Very Rare specimen to get
.
The
Lepidostrobus
is the generic name for the cones of arboresent lycopsid. It corresponds closely in structure with the fertile spike of the living
Selaginella.
The spore-bearing leaves are attached to   a central axis in a crowded spiral arrangement, and their outer ends curve over so as to form an imbricated, diagonally arranged pattern, resembling that of the stem itself. The
Lepidostrobus
cones produced spores and megaspores.
Systematic:
Division:          Tracheophyta (Lycoposida)
Class:              Lycopodinae
Order:              Lycophodiales
Family:            Lepidodendraceae
Genus:
Lepidostrobus
Brongniart (1828)
Species:
Lepidostrobus variabilis
Lidney & Hutton
Lepidodendron
(also known as the "Scale tree") is an extinct genus of primitive, vascular, arborescent (tree-like) plant related to the Lycopsids (club mosses). It was part of the coal forest flora. They sometimes reached heights of over 30 metres (100 ft), and the trunks were often over 1 m (3.3 ft) in diameter, and thrived during the Carboniferous period. Sometimes called "giant club mosses", this is actually not correct as they are actually closer to quillworts than to club mosses. The closely packed diamond-shaped leaf scars left on the trunk and stems as the plant grew provide some of the most interesting and common fossils in Carboniferous shales and accompanying coal deposits. These fossils look much like tire tracks or alligator skin. The scars, or leaf cushions, were composed of green photosynthetic tissue, evidenced by the cuticle covering and being dotted with stomata, microscopic pores through which carbon dioxide from the air diffuses into plants. Likewise, the trunks of
Lepidodendron
would have been green, unlike modern trees which have scaly, non-photosynthetic brown or gray bark.
Lepidodendron
has been likened to a giant herb. The trunks produced very little, if any, wood. Most structural support came from a thick, bark-like region. This region remained around the trunk as a rigid layer that did not flake off like that of most modern trees. As the tree grew, the leaf cushions expanded to accommodate the increasing width of the trunk. The branches of this plant ended in cone-like structures.
Lepidodendron
did not produce seeds like many modern plants. Instead, it reproduced by means of spores. It is estimated that these plants grew rapidly and lived 10–15 years. Some species were probably monocarpic, meaning they reproduced only once toward the end of their life cycle.
Lepidodendron
likely lived in the wettest parts of the coal swamps that existed during the Carboniferous period. They grew in dense stands, likely having as many as 1000 to 2000 giant clubmosses per hectare. This would have been possible because they did not branch until fully grown, and would have spent much of their lives as unbranched poles. In its juvenile stages, the trunk was supported by grass-like leaves that grew straight out of the trunk. By the Mesozoic era, the giant clubmosses had died out and were replaced by smaller clubmosses, probably due to competition from the emerging woody gymnosperms and other plants.
Lepidodendron
is one of the more common plant fossils found in Pennsylvanian (Late Carboniferous) age rocks. They are closely related to other extinct genera,
Sigillaria
and
Lepidendropsis
.
In the 19th Century, due to the reptilian look of the diamond-shaped leaf scar pattern, petrified trunks of
Lepidodendron
were exhibited at fairgrounds as giant fossil lizards or snakes. The name
Lepidodendron
comes from the Greek
lepido
, scale, and
dendron
, tree.