Answer:
question 1 answer)
Explanation:
it means that they have a close relationship by their reverse. how exactly? here:
photosynthesis: CO2 + Energy = Glucose + O2
photosynthesis: CO2 + Energy = Glucose + O2cellular respiration: O2 + Glucose = CO2 + Energy
as you see here, they're same but opposite.
Answer:
Chloroplasts
Explanation:
Chloroplasts are lens-shaped organelles that contain, chlorophyll, which is a photosynthetic pigment that traps light energy. The light energy is harvested to provide energy for the reactions of photosynthesis.
They are found in the leaf cells of green plants
I found the exercise on the internet. Attached is a picture of the <span>statements and the bins.
Operon is not transcribed:
-trp operon: tryptophan present (tryptophan works as an inhibitor of the operon)
-lac operon: lactose absent (lactose works as the trigger for the operon)
Operon is transcribed but not sped up by positive control:
-trp operon: tryptophan absent </span>(tryptophan works as an inhibitor of the operon, when absent the operon is active)
-lac operon: lactose present, glucose present (lactose works as the trigger for the operon, but when glucose is present, the operon activity remains only at basal level)<span>
Operon is transcribed quickly by positive control:
-lac operon: lactose present, glucose absent </span>(lactose works as the trigger for the operon, but when glucose is absent, the operon activity is at its maximum activity)
Abrasion, plucking, deposition, and physical weathering are the glacial actions which can be observed all over the park.
Explanation:
When the huge ice masses slope down to fall over the land surface during a glacier, many glacial actions or processes take place which defines the landforms formed on the surface. These actions include abrasion, plucking, deposition, and physical weathering.
Abrasion is an erosive process which scrapes the surface of ice rocks and other frozen rocky material beneath the ice and causes striations over the rocks.
Plucking also an erosive process plucks the frozen rocks beneath the ice surface.
Physical or freeze-thaw weathering causes water to enter the cracks in the rocks when the temperature increases. This water enters inside and freezes inside when the temperature goes down. This repeated melting and freezing of water destabilizes the rocks and will break the rocks.
These materials which are worn off are transported and deposition on the land surface when the glacier settle down.
Longshore drifts occur along coastlines and brings materials along the coast when waves move at an angle with the coastline.