Answer:
1. True
Explanation:
From a certain depth, most of the carbonates dissolve, but the shells of the most resistant foraminifera do not. It is the LISOCLINE
.
From a certain depth, carbonates and microfossils dissolve completely beyond lysocylin. It is the CALCITE COMPENSATION LEVEL (CCD)
.
In areas deeper than the CCD, only clay or siliceous sediments are deposited and carbonates and carbonated fossils are absent
.
Lysocline and CCD vary in depth today in each ocean, being greater in the tropical belt (up to 5000 m)
. The CCD for the same latitude has varied throughout geological time
.
Answer:
The climate of any particular place is influenced by a host of interacting factors. These include latitude, elevation, nearby water, ocean currents, topography, vegetation, and prevailing winds. The global climate system and any changes that occur within it also influence local climate.
The biosphere, also called the ecosphere, is the natural environment of living organ- isms and is the complex biological epidermis of the Earth whose dimensions are not precisely defined. It consists of the surficial part of the lithosphere, a lower part of the atmosphere, and the hydrosphere.
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The answer would be "History being told by one person at a time"