I think the answer is either b or c
Unfortunately I don’t think your question was typed correctly unfortunately. But I’ll try my best!
Interphase, Prophase, Metaphase, Anaphase, Telophase and Cytokinesis (these tend to be lumped together in my classes.)
I remember them in a weird way.
Interphase- In rest/chaos (depending on how you want to look at it). The DNA is all jumbled up inside the nucleus, just chilling and doing its normal stuff.
Prophase-proper. The DNA now decides hey, time to get our stuff together and get into our chromosomes.
Metaphase-middle. The chromosomes line up at the metaphasal plate, ready to get splitting (and a bunch of other junk, depending on which mitosis we’re talking about.)
Anaphase- apart. Now that the chromosomes have done their duties, we now have chromaTIDS (tidbit chromosomes) who get pulled to opposite ends of the cell.
Telophase/Cytokinesis- “tear apart” and a new cytoplasm! Now we’ve got new daughter cells!
The right answer is pectinated muscles.
The right atria extends between the two cellar veins. It is of rounded aspect, but for the simplification of its description, it is assimilated to one cube having 6 walls:
Anterior wall
A lower wall
A posterior wall
A top wall
An inner or septal wall
An outer or straight wall: relatively thin, has muscle thickenings: pectinated muscles. This is the preferred route of choice for cannulations during cardiac surgery under extracorporeal circulation.
Answer:
i saw that they were called whisk ferns
Explanation:
Answer:
In evolutionary studies, absolute dating can be described as a method which scientists use to date any material that they find. Relative dating is a method in which scientists try to puts the geological events in a relative order. In absolute dating, the exact age of the rock will be calculated by the scientist. In relative studies, the scientist will try to place the rock in the best geologic time in which the rock might have existed.
The most common method for absolute dating is the method of radiometric dating. Radioactive minerals present in the rock act as geologic time which are determined by the scientists.