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Science
Olympiad
Division
(Phylum) Magnoliophyta |
Flowering
plants or angiosperms (Magnoliophyta) make their first
unmistakable appearance during
the Early Cretaceous (140 MYA) (Kenrick & Davis 2004, p.
195). Thus, angiosperms appear 300
million years after the first vascular plants and
220 million
years after the first seed plants (Willis & McEwain, 2002,
p 156). Angiosperms underwent a rapid adaptive radiation soon
after their first appearance. In fact, angiosperms
became the dominant flora across the globe by the Paleogene a
mere 70 million years after their first appearance. Flowering
plants
continue
to dominate the world’s
flora today; extant pteridophytes species number 10,000,
gymnosperms 750,
and angiosperms up to 300,000 species. These new
seed plants possessed a number of important characteristics that
separate
them from other seed plants.
A New Kind of Seed Plant
Flowering plants evolved distinctive characteristics that
help to define this plant division. Angiosperms possess flowers,
develop fruits, contain specialized conducting cells in their
vascular tissues, develop a double-layered seed coat, exhibit
a distinctive column-like structure in their pollen grain walls,
and undergo double fertilization during their life cycle.
New Reproductive Stategies
New reproductive strategies
helped angiosperms become a great success and diversify into
the forms we know
today.
In angiosperms male and female structures develop within flowers.
The pistil is the central, female organ of the flower and
typically consists of an ovary with ovules, a style and stigma.
The stamen is the male part of a flower and typically consists
of a filament or stalk topped with pollen producing anthers.
When
pollen comes into contact with a flower's stigma the growth
of a pollen tube is activated. Each pollen grain carries
two sperm. One sperm fertilizes
an egg in the ovule; the other sperm unites with two haploid
cells in the same ovule. This process is known as double
fertilization and is an important adaptation found in angiosperms.
The fertilized
egg will undergo cell division to become
a zygote and then an embryo. The second fertilization results
not in offspring, but rather the development of endosperm,
which acts as a nutrient for the embryo. Cells in
the endosperm have three sets of chromosomes.
Endosperm not only serves as an important food source for
the embryos of flowering plants it also is important to
other animals. Humans depend upon the endosperm of rice,
wheat, and corn. Recent research indicates the endosperm
may also
act as a fertilization sensor helping to abort embryos
of incompatible crosses (Juniper & Mabberley 2006, p.27).
A seed is formed when
the endosperm and the embryo become enveloped in a part
of the ovule that hardens into the seed coat. The ovary
or other parts of the flower in angiosperms develop into
a fleshy
fruit
surrounding the seeds. Many
organisms such as birds, bats, and insects have coevolved
to help pollinate
angiosperms. The fleshy fruits of angiosperms are an
adaptation for seed dispersal. Many animals use the fruit
as a food
source, which results in the dispersal of seeds encapsulated
within
a natural fertilizer!
Monocots & Dicots
Traditionally angiosperms are
divided into the monocotyledons and dicotyledons. Today angiosperms
are divided into the monocots, eudicots, and magnoliids. Monocots
and eudicots are monophyletic groups. Eudicots contain
most of the dicots. It is useful to known the major differences
between monocots and dicots (eudicots & magnoliids) when studying
both extinct and extant plants.
Monocots have one cotyledon
(seed leaf) at germination. Monocots usually have
flower parts
in
threes,
one aperture or furrow on their pollen, parallel leaf venation,
a scattered arrangement of vascular bundles, and usually
no secondary woody growth. Grasses
and palms are well known examples of monocots. Petrified
plam wood or Palmoxylon is the state stone for Texas
and the state fossil for Louisiana. The state stone for
Mississippi is petrified wood and much of the fossil wood
found in the state is Palmoxylon.
Dicots
have
two cotyledons when they germinate. Today there are six
times as many dicots as monocots. Dicots usually have flower
parts
in fours or fives, possess three
apertures
on
their
pollen (except the magnoliids, which have one), netlike leaf
venation,
vascular bundles arranged in rings, and commonly have secondary
woody growth (Willis & McElwain, 2002, pp. 156-157).
Woody dicots possess eustele stems; a central pith surrounded
by secondary wood and bark. Woody deciduous
trees such as
oak,
elm,
and maple
are good examples
of dicots. When looking at permineralized wood in cross-section
one can quickly distinguish between gymnosperms and angiosperms
with a 10x loupe.
New Vascular Tissue
Most angiosperms have
two cell types that are distinctly different in size. The
large, water conducting cells, are called vessels; the smaller
diameter, more abundant cells are fibers. Gymnosperm
wood is made of small diameter tracheids. Tracheids are more
easily
seen with a 20x loupe. Angiosperms also have tracheids for
water conduction. Among the angiosperms we can also distinguish
between dicots and
monocots.
Dicots
have
their
vessels and fibers arranged in rings while monocots have
their vascular bundles scattered throughout the stem giving
a speckled appearance even to the naked eye (Kenrick & Davis,
2004, p. 74).
A New Age of Plants
The
first angiosperms had small
seeds, which may indicate they were
small herbaceous weedy generalists (Willis & McElwain,
2002, p162). The lack of angiosperm wood in the early Cretaceous
would also support the idea that the first flowering plants
were small herbaceous plants. Fossil evidence from flowers,
leaves and pollen suggests that
dicots evolved
before monocots.
Cladistic
analysis indicates a close relationship between Bennettitales,
Gnetales and angiosperms (Willis & McElwain, 2002, p. 184).
The
diversification of flowering plants during the Cretaceous
helps to mark a significant change in the world's flora.
Paleozoic
flora was dominated by ferns and clubmosses (Paleophytic
flora). The Paleophytic flora gave way to a Mesophytic
flora during the Triassic period. Woody seed-bearing plants
and their relatives dominated Mesophytic flora. Thus, the
change from Paleophytic to Mesophytic represented a change
in reproductive strategy; from spore producers to seed
producers. Conifers, cycads, and ginkgoes diversified during
this time and dominated the landscape. Flowering plants
first emerge during the Early Cretaceous and undergo a
great adaptive radiation during the Middle Cretaceous.
Flowering plants quickly became a major constituent of
species diversity and the world entered the third great
age of plant life known as the Cenophytic by the Late Cretaceous
(Kenrick & Davis,
2004, p. 143).
The
transition from Mesophytic to Cenophytic represents a
change
in reproductive strategies. Gymnosperms and their relatives
relied mostly on wind pollination and bore naked seeds
clustered in cones or on the end of stocks. Flowering
plants coevolved with animal pollinators, underwent double
fertilization,
and
encased
seeds in a fleshy ovary that encouraged seed dispersal.
Our modern plant world is a continuation of the Cenophytic
age of plants.
Science Olympiad Fossil Event
The 2016 Science Olympiad Fossil List includes three genera under the phylum Anthophyta (Flowering Plants): Acer, Populus, and Platanus. Acer is the
maple genus. Today maples are an important part of the
deciduous hardwood forests of North America. Maples are
important economically as a source of hardwood and
syrup. Maples are also used as ornamental shade trees
(Elias, 1980, p. 775). Populus includes familiar plants such as poplar, cottonwood, and aspen trees. Platanus includes sycamore and plane trees. In the section titled "Other",
petrified wood is listed, which does include flowering plants.
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Fraxinus sp.
Grassy
Mountain Basalt
Miocene
Grassy Mountain, Malheur Co, OR
12 cm x 10 cm
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Schinoxylon sp.
Green River Formation
Eocene
Blue Forest, Wyoming
12 cm x 10 cm
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Palmoxylon sp.
Catahoula Formation
Oligocene
Rapides Parish, Louisiana
11 cm x 9 cm
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Palmoxylon sp.
Bridger Formation
Eocene
Farson, Wyoming
4 cm diameter
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Palm Fiber & Roots
Palmoxylon & Rhizopalmoxylon
Denver Formation
Paleocene
South Platte River Quarry
Denver, Colorado
19 cm x 17 cm
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Palm
Trunk
Palmoxylon
Denver Formation
Paleocene
South Platte River Quarry
Denver, Colorado
12 cm x 11 cm
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Sycamore
Platanus sp.
Denver Formation
Paleocene
South Platte River Quarry
Denver, Colorado
20 cm x 15 cm
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Maple
Acer sp.
Denver Formation
Paleocene
South Platte River Quarry
Denver, Colorado
12 cm diameter
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Fig
Ficus sp.
Miocene
Swartz Canyon, Oregon
12 cm diameter
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Oak
Quercus sp.
Columbia Group Basalts
Miocene
Vantage, Washington
16 cm x 12 cm
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Colorado
Palm Trunk Close-Up
Showing Vascular Bundles
20x |
Vantage Oak Close-Up
Showing Vessels
10x |
Balloon Vine
Cardiospermum coloradensis
Green River Formation
Eocene
Bonanza, Utah
7 cm long
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Cedrelospermum sp.
Miocene
Randecker Maar Esslingen, Germany
Leaf 4 cm long, Seed 1 cm long |

Sycamore Leaf
Platanus wyomingensis
Green River Formation
Eocene
Uintah County, Utah
11 cm wide x 10 cm tall
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Oak
Leaf
Quercus
dayana
Sucker
Creek Formation
Miocene
Succor Creek
Malheur County, Oregon
6 cm long x 2.2 cm wide
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Poplar Leaf with Insect Damage
Populus wilmattae
Green River Formation
Eocene
Bonanza, Utah
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Bibliography
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Elias, T.S. (1980). The
Complete Trees of North America. Van Nostrand Reinhold
Company: New York.
Juniper, B.E. & Mabberley, D.J. (2006). The Story of the Apple.
Timber Press, Oregon.
Kenrick,
P. and Davis, P. (2004). Fossil Plants. Smithsonian
Books: Washington.
Willis,
K.J. & McElwain, J.C. (2002). The Evolution of
Plants. New York: Oxford University Press. |
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