Biology, 16.09.2019 00:20 celi1236

How would a paleozoic ocean be different than an ocean today? how would it be the same?

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Answer from: joel53

Different: different species, environments in the ocean, behaviors of animals

Answer from: dontworry48

There would be a lot of difference between Paleozoic ocean and the ocean which we see today. Value Zoe question occur approx. 300 million years ago. A lot of change has occurred during the course of duration.

The police question had contained much rich biodiversity in it as compared to the oceans now. Most of the animals become extinct. The element H2O is same. It means the water are same when compared.

The presence of CO2 in the atmosphere could have affected the ocean water quality. The position of ocean and continent has also changed when compared with past. Ocean used to occur in the northern hemisphere earlier but it is shifted to the southern hemisphere now.

Answer from: Quest

Mantle convection is the slow creepingmotion of earth's solid silicate mantle caused by convection currents carrying heat from the interior to the planet's surface.[1][2] the earth's surface lithosphere, which rides atop the asthenosphere (the two components of the upper mantle), is divided into a number of plates that are continuously being created and consumed at their opposite plate boundaries. accretion occurs as mantle is added to the growing edges of a plate, associated with seafloor spreading. this hot added material cools down by conduction and convection of heat. at the consumption edges of the plate, the material has thermally contracted to become dense, and it sinks under its own weight in the process of subduction usually at an ocean trench.[3]this subducted material sinks through the earth's interior. some subducted material appears to reach the lower mantle,[4] while in other regions, this material is impeded from sinking further, possibly due to a phase transition from spinel to silicate perovskiteand magnesiowustite, an endothermic reaction.[5]the subducted oceanic crust triggers volcanism, although the basic mechanisms are varied. volcanism may occur due to processes that add buoyancy to partially melted mantle causing an upward flow due to a decrease in density of the partial melt.secondary forms of convection that may result in surface volcanism are postulated to occur as a consequence of intraplate extension[6] and mantle plumes.[7]it is because the mantle can convect that the tectonic plates are able to move around the earth's surface.[8]mantle convection seems to have been much more active during the hadean period, resulting in gravitational sorting of heavier molten iron, and nickel elements and sulphides in the core, and lighter silicate minerals in the mantle.

Answer from: Quest

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