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Amanda [17]
3 years ago
5

How does fertilization affect the chromosome number of a zygote?

Biology
1 answer:
olya-2409 [2.1K]3 years ago
4 0

Answer:

Fertilization is the fusion of gametes to form the zygote. ... Fertilization allows restoring of the chromosome number of the species as the two nuclei of gametes fuse together. Therefore, the number of chromosomes in the zygote is twice the number of chromosomes in gametes.

Explanation:

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Which receptors adapt most slowly?
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2) nociceptors
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3 years ago
A protein that contains more isoleucine, phenylalanine and leucine than asparagine, lysine and arginine is most likely ________.
Snezhnost [94]

Answer:

The correct answer is: Hydrophobic, Hydrophobic.

Explanation:

  • Proteins are made up of polypeptide chains which are formed by the polymerization of amino acid molecules, linked together by peptide bonds.
  • The amino acids can be broadly classified into non-polar and polar.
  • The non-polar amino acids can be defined as those amino acids whose side chains possess hydrocarbon molecules only. They do not possess any charge and are incapable of forming hydrogen bonds with water molecules. They tend to avoid water and so they tend to remain buried into the interior of a protein. Examples can be illustrated as Leucine, Valine, Isoleucine, Phenylalanine, etc.
  • The polar amino acids can be defined as those amino acids whose side chains either possess a charge (positive or negative) or a hydroxyl group which is capable of forming hydrogen bonds with water molecules. As they tend to form hydrogen bonds with water molecules they are usually found on the surface of the proteins. Examples can be illustrated as Lysine, Arginine, Serine, Asparagine, etc.
6 0
3 years ago
Which two types of clouds often produce precipitation?
eduard

Answer:

Altostratus and Cumulus.

Explanation:

6 0
2 years ago
What is the most common type of organic molecule?
dusya [7]

Answer:

I am not certain but I think carbohydrate

3 0
3 years ago
Read 2 more answers
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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