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likewise the warming of the eocene is linked to high atmospheric co2 levels and cooling towards the late oligocene was sequentially reduced co2 levels.
likewise the warming of the eocene is linked to high atmospheric co2 levels and cooling towards the late oligocene was sequentially reduced co2 levels.
we evolve from prosimians into true primates in the eocene and oligocene. conditions of the eocene were high levels of co2 and high temps all over the planet.
we evolve from prosimians into true primates in the eocene and oligocene. conditions of the eocene were high levels of co2 and high temps all over the planet.
new bats of the average oligocene phosphorites of quercy , france . proceedings of the academy of sciences in paris , 310, 1131 –1137 .
nové netopýrů průměrných oligocene fosforitů z quercy , francie . sborník akademie věd v paříži , 310, 1131 -1137 .
our results demonstrate that pco2 ranged between 1000 to 1500 parts per million by volume in the middle to late eocene, then decreased in several steps during the oligocene, and reached modern levels by the latest oligocene.
our results demonstrate that pco2 ranged between 1000 to 1500 parts per million by volume in the middle to late eocene, then decreased in several steps during the oligocene, and reached modern levels by the latest oligocene.
re: "likewise the warming of the eocene is linked to high atmospheric co2 levels and cooling towards the late oligocene was sequentially reduced co2 levels."
re: "likewise the warming of the eocene is linked to high atmospheric co2 levels and cooling towards the late oligocene was sequentially reduced co2 levels."
in this case it is the northward movement of the indian plate towards asia that is proposed as the source of the slow, slow ramp up of atmospheric co2 (and associated warming) and the slow,slow loss of co2 that progressed into the oligocene and gave the world antarctic glaciation.
in this case it is the northward movement of the indian plate towards asia that is proposed as the source of the slow, slow ramp up of atmospheric co2 (and associated warming) and the slow,slow loss of co2 that progressed into the oligocene and gave the world antarctic glaciation.
