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vodomira [7]
3 years ago
7

Exposure to cocaine during pregnancy leads to increased risk of: select one:

Biology
1 answer:
uysha [10]3 years ago
8 0
I believe it's A. Premature Birth (though they all seem pretty believable)
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Polygamy is practiced in some parts of the world, while monogamy is practiced in others. people who believe that polygamy or mon
drek231 [11]

Some regions of the world practice polygamy, while others only monogamy. People who consider polygamy or monogamy to be abnormal behaviors are not using their sociological imagination.

<h3>What does sociological imagination entail?</h3>
  • an understanding of the connection between our social environment and who we are as individuals.
  • difficulties that people experience on a personal level rather than as a result of their social standing. public matters
  • Simply described, sociological imagination is the capacity to relate smaller societal problems to more significant human problems.
  • It is crucial to have a social imagination since it aids in comprehending and recognizing the numerous facets of society.
  • Additionally, a person's troubles will reflect societal policies.
<h3>What are the sociological imagination's four elements?</h3>

The historical, cultural, structural, and critical sensibility are four interrelated ones that make up sociological imagination.

learn more about sociological imagination here

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4 0
2 years ago
At what point did the corn yield increase the most as the amount of fertilizer increased?
Yakvenalex [24]

Here's li^{}nk to the answer:

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5 0
3 years ago
Which of the following is a function of the nervous system?
IrinaVladis [17]
I believe the correct answer from the choices listed above is option C. One function of the central nervous system would be signaling muscle tissues to contract.  <span>It is the </span>system<span> of the body that receives and processes all information from all parts of the body. It sends signals to the body parts.</span>
3 0
3 years ago
What is the most important factor in successful learning
alukav5142 [94]

listening and understanding the subject

8 0
3 years ago
How do you refer to how the average temperature of the atmosphere has changed over geological time?
Verizon [17]

Answer:

Explanation:

A non-antagonistic environment was essential for the advancement of life as far as we might be concerned. Was there fluid water? Was there outside on which life could grab hold? Earth's livable surface today is positively not quite the same as it was 4.6 Bya when it originally dense out of our Sun's dusty, turning cloud. We have next to no excess proof of Earth's covering during its initial 500 million years — simply a small bunch of strong zircon grains from the Jack Hills combination in western Australia (Maas et al. 1992, Wilde et al. 2001). Notwithstanding their minuscule size, bolted inside every zircon's precious stone grid is a noteworthy record of occasions back 4.4 Bya. Their science, distinguished by particle radiates only a couple microns wide, recommend they shaped as a component of light covering and within the sight of fluid water (Mojzsis et al. 2001, Peck et al. 2001, Wilde et al. 2001).  

On the off chance that fluid water and raised covering existed so right off the bat in Earth's set of experiences, was life present too? There is carbon isotope proof for life on the planet's most seasoned known volcanic-sedimentary rocks (3.7–3.9 Bya) in the Isua rock formation of West Greenland (Rosing 1999). Sedimentary rocks saved in deepwater, underneath the photic (light-infiltrated) zone, contain sloppy, carbon-rich layers with a carbon-isotope signature like natural rich muds of the cutting edge sea. As in the cutting edge sea, these carbon-rich layers might have aggregated as planktonic microscopic organisms at the surface kicked the bucket and settled to the sea depths. Had life developed by 3.7 Bya, however the proof from Greenland indicates that these living things might have been photosynthetic, flourishing in light-filled surface waters.  

Life before 3.9 Bya is more speculative, in light of the fact that more seasoned rocks were wrecked by the late hefty shooting star barrage (LHB) that likewise cratered our Moon. It could be that extremophiles, which we currently comprehend to live at temperatures up to 120°C (Kashefi and Lovley 2003) and profundities in excess of 3 km (Lin et al. 2006), existed before 3.9 Bya and were fit to endure the LHB by colonizing profound natural surroundings (Abramov and Mojzsis 2009). Then again, there is adequate proof that salt marsh environments endure a time of hefty shooting star siege between 3.5–3.2 Bya — impacts 10 to multiple times greater than the Cretaceous-Tertiary (K-T) occasion that produced strong torrents (Byerly et al. 2002). It seems superfluous to accept that life "paused" to advance until after the LHB occasions, nor that extremophiles were the lone structures fit to endure times of substantial effects.  

Regardless of whether life emerged previously or after the LHB, it did as such without the assistance of free oxygen. It is grounded from sedimentary rocks and paleosols that free oxygen didn't amass in the air until after 2.5 Bya (Rasmussen and Buick 1999, Farquhar et al. 2000, Pavlov and Kasting 2002, Holland 2006). Truth be told, the last ascent to present day air levels happened just ~580 million years prior (Mya), permitting complex life to broaden ashore (Des Marais et al. 1992, Knoll 1992, Canfield and Teske 1996, Narbonne and Gehling 2003).

8 0
2 years ago
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