thaumaturgy
Well-Known Member
That is very true; however, I would imagine that ferns are a far studier plant then say a water lily. I would suggest that you visit a garden after a torrential rainstorm with hail and high winds. It isn't a pretty sight. The flowers are gone. What survived as fossils are the sort of things that were not delicate. Pine cones and needles are not as delicate as flowers and leaves. They would look like something and not a mashed ground up mass.
But, Little Nipper, we aren't talking about coalifying the flowers, but rather the flowering plants.
A flowering plant, even when the flowers are stripped off is still a flowering plant.
The structures preserved in coals include ways to identify whether a plant was angiospermous or gymnospermous.
(Emphasis added)Seyler (1928, 1929) as well a Hickling and Marshall (1932, 1933) have studied various microstructures of vitrinite of European Carboniferous coals and identified even the species of plants from which the coals were derived. In the Gondwana coals, little work has been done on similar lines. However, Ganju (1955) has noted that bark formed an important constitutent of vitrinites of Indian coals in which he a observed well-preserved secondary bark tissue. He also observed wood, mainly of gymnospermous origin, as a dominant constituent of vitrinites of Indian coals and has described well-preserved woody structures including bordered pits characterisitcs of gymnospermous wood (Coal Petrology, 3rd Ed., 1982, Stach et al.)
Those should be found in abundance in Carboniferous coal swamps if they were present at the time in the same abundance.
Sure some things are going to prefer some environments over others, but if a Flood-Literalist wishes to argue this point, you have to explain why some swampy areas have flowers today but not then.
But further, swamps are the only places where coal formed. Forest swamps and raised bogs also formed coal deposits. A variety of climates could support coal-forming conditions, however humidity helped. Standing water with the proper anoxic conditions was important.
But also important to remember is that some coal is allochthonous. That means it is made up of plant materials that have been transported some distance from where they originally grew. Usually these are too rich in mineral matter to be good seams for mining, but they also indicate that just because you have a coal does not mean you have it where the plants originally grew. (There are apparently driftwood deposits from Siberia that are in Spitsbergen today.)
Coal forms in 4 "swamp" types usually:
- Open water areas
- Open reed swamps
- Forest swamps
- Moss swamps
Coals tell us a lot about what was where and when.
Now we can find angiospermous (flowering) plant material in younger coals, like this one.
So we need to know why some earlier "times" in the geologic record don't show any angiospermous wood.
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