One of the main characteristics of secondary granules in the neutrophilic granulocyte cytoplasm is that secondary granules will become pink/tan and will cause the basophilic color to lighten.
Promyelocytes, metamyelocytes, and myelocytes are the precursors of neutrophils, which make up the majority of the white blood cell population. The immature neutrophils are usually found only in the bone marrow.
Myeloid maturation sequence is the next stage of myelocyte. The cytoplasm of this cell starts to produce specific, secondary granules. If the cell is destined to be a neutrophil these secondary granules will be pink/tan and will further cause the basophilic color to lighten and break up. At the beginning of neutrophilia, these secondary granules are most obvious in the golgi area.
As the cell matures closer to a metamyelocyte, they fill the entire cytoplasm. While the cytoplasm shifts to producing secondary granules it also loses the prominence of its primary granules.
Learn more about neutrophils here :
brainly.com/question/27960149
#SPJ4
25% will have bb when crossing u have 1 BB 2 Bb 1 bb
Metamorphic rocks are identified by the types of minerals they contain and their texture. Examples of sedimentary rocks changing to metamorphic rock as a result of heat and pressure are limestone changing to marble, and shale changing to slate.
38 ATP molecules are produced
Good luck! hope this helps (:
Clastic sedimentary rocks
Most rocks that form from fragmental rock particles are classified as clastic sedimentary rocks.
Clastic sedimentary rocks are rocks that are formed by weathering processes due to exposure of pre-existing rocks to wind, ice, and water which breaks down the pre-exsiting rocks into chunks, pebble, sand, and smaller rock particles. Types of clastic sedimentary rocks include; conglomerate, breccia, shale and sandstone.
