Write a short note on asexual reproduction in
bread mould

During Asexual reproduction, in the interior side  of Sporangium spores are made by mold and spreading of more mold occurs and  Sporangium will be breaking during the time, when the spores are ready for leaving out.

Explanation:

The formation of spores is the asexual reproduction method that occurs in fungi which is a non flowering plant and bacteria. Many number of smaller and tiny spores that are tough, round shaped and microscopic, are produced by parent plants that has the ability to grow into many newer plants in asexual reproduction method only under certain conditions.   Multiple number of spores in the sacs of Rhizopus that is called as sporangia. Te structure of these sporangia is like a knob and these are  are present at the top of  hyphae which is like a thread.

When these sporangia bursts, the spores are scattered by rain, wind or insects and under suitable conditions develop into a new Rhizopus plant, when they fall on a suitable substance like bread. When a break occurs in these sporangia, scattering of these spores occurs and these develop into a new plant under some suitable conditions, when these falls on a substance say for an instance bread.

events in order:

1.       vishnu schist

2. zoroaster granite

3. bass limestone

4. hakatar   shale

5. igneous intrusion

6. shinumo quartzite

7. dox sandstone

8. tapeats limestone

9. bright angel shale

10. muav limestone

11. temple butte limestone

12. redwall limestone  

nonconformity

answer: the unkar group shows angular unconformity because the layers are turned at angle.

unconformity

answer: specifically the angular unconformity occurs between the cambrian and precambrian rocks. the dox sandstone, shinumo quartzite, hakatar shale, and bass limestone have been filled. an angular unconformity occurs between the cambrian and precambrian rocks. the dox sandstone, shinumo quartzite, hakatar shale, and bass limestone have been filled.

disconformity

answer: the disconformities aremarked irregular lines between the sedimentaryrocks layers.