The accumulation of partially decayed plant material is called Pea Peat may be covered with
sediment and placed under extreme andss With time and pressure peat may be compressed into
boaAu tread (Paragraph 2)The rate of fossil fuel formation was great during the period. The
lands were covered by Carbon accross and the climate was ool Zdanne so this favored year round
growth. The Svps dominated the landscape and hence created most of the coal. Also present but
not in type of seed plants. abundance were the (Paragrpah 3) which tree dominated in the
Carboniferous? trees Another tree, Giant Horsetails, was also abundant. These were both svps, so
they still had external fertilization (released spores and sperm into the water). They flourished in
this tropical/wet climate. (Pg 401, paragraph 2) What happened to the climate and hence the svp
trees at the end of the \"R Carboniferous? climakt tin coz t ceel ca med agey in The water
receded so the spores and sperm croaked Only pmaALlycDonytes relatives of SVP trees remain
today. One group of Gymnosperms, survived to today. They evolved pollen to transport sperm
and so moved to internal fertilization. They were able to take over the drying landscape at the
end of the Carboniferous!!!!!
Solution
Ques-1:
The accumulation of partially decayed plant material is called peat. Peat may be covered with
sediment and placed under extreme pressure. With time and pressure peat may be compressed
into \"peat bog\" or mire
Ques-2
The rate of fossil fuel formation was great during the carboniferous period. The lands were
covered by peat (dead trees & dead plant organisms) and climate was cold & damped. So this
favored year round growth. The SVPs dominated the landscape and hence created most of the
coal. Also present but not in abundance were the vascular -angiosperm type of seed plants.
The accumulation of partially decayed plant material is called Pea Pe.pdf
1. The accumulation of partially decayed plant material is called Pea Peat may be covered with
sediment and placed under extreme andss With time and pressure peat may be compressed into
boaAu tread (Paragraph 2)The rate of fossil fuel formation was great during the period. The
lands were covered by Carbon accross and the climate was ool Zdanne so this favored year round
growth. The Svps dominated the landscape and hence created most of the coal. Also present but
not in type of seed plants. abundance were the (Paragrpah 3) which tree dominated in the
Carboniferous? trees Another tree, Giant Horsetails, was also abundant. These were both svps, so
they still had external fertilization (released spores and sperm into the water). They flourished in
this tropical/wet climate. (Pg 401, paragraph 2) What happened to the climate and hence the svp
trees at the end of the "R Carboniferous? climakt tin coz t ceel ca med agey in The water
receded so the spores and sperm croaked Only pmaALlycDonytes relatives of SVP trees remain
today. One group of Gymnosperms, survived to today. They evolved pollen to transport sperm
and so moved to internal fertilization. They were able to take over the drying landscape at the
end of the Carboniferous!!!!!
Solution
Ques-1:
The accumulation of partially decayed plant material is called peat. Peat may be covered with
sediment and placed under extreme pressure. With time and pressure peat may be compressed
into "peat bog" or mire
Ques-2
The rate of fossil fuel formation was great during the carboniferous period. The lands were
covered by peat (dead trees & dead plant organisms) and climate was cold & damped. So this
favored year round growth. The SVPs dominated the landscape and hence created most of the
coal. Also present but not in abundance were the vascular -angiosperm type of seed plants
