there is no word called carboniferous
carbon is an element that has a grayish blackish color. its most common molecule is carbon dioxide. if you add that to the time scale, the carbon dioxide will add up in the atmosphere that we live in. ifyou add 2010 then you havethe amount of carbon dioxide in the atmosphere in the year 2010... which is alot. and people are tryingto reduce carbon emissions.
paleozoic
i need plus 2 biologly group time table for 2010
The dominant organisms during the carboniferous time period were plants. They were large, vascular, land plants that sometimes grew to be one hundred feet or more.
During the Carboniferous period, the atmosphere had higher oxygen levels compared to today. The increase in oxygen levels during this time supported the growth of large insects and amphibians. The high concentration of carbon dioxide in the atmosphere during the Carboniferous period also contributed to the warm climate and lush vegetation of that time.
by the time they finish.
yes because of all the CARBON-iferous i am halariouse
The largest sections on the geologic time scale are Precambian (which includes the Hadean, Archean and Proterozoic frames), the Phanerozoic (which includes the Palaeozoic, Mesozoic [the well known dinosaur era] and the Cenozoic [the most modern time frame]). After that, take your pick of the smaller subsections of the time scale for the last one. No, actually the answer above states three eras. There are 4, the Precambrian, the Paleozoic with Cambrian, Ordovician, Silurian, Devonian, Carboniferous periods, the Mesozoic with the Triassic, Jurrasic and Cretacaous periods and the Cenozoic with Tertiary and Quaternary.
Some dangers in the Carboniferous period included volcanic activity, which could lead to eruptions and the release of toxic gases. Additionally, the high levels of oxygen in the atmosphere during this time could have increased the risk of wildfires. Lastly, the presence of large predatory insects and amphibians could have posed a threat to other organisms.
The highest oxygen level in Earth's history occurred during the Carboniferous Period, approximately 300-360 million years ago. This period is often referred to as the "golden age of insects" due to the size and diversity of insect species during this time.
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Paleozoic Era- Cambrian, Ordovician, Silurian, Devonian, Carboniferous, Permian Mass Extinction (Permian-Tertiary) 248 mya Mesozoic Era- Triassic, Jurassic, Cretaceous Mass Extinction (K-T) 65 mya Cenozoic- Tertiary, Quaternary
The Carboniferous period occurred approximately 359 to 299 million years ago, during the Paleozoic Era. It is characterized by the extensive development of forests and swampy environments, which contributed to the formation of significant coal deposits. This period is also notable for the diversification of amphibians and the early evolution of reptiles. The Carboniferous is typically divided into two subperiods: the Mississippian and the Pennsylvanian.