Tapetum
Pollen grains are tiny, microscopic structures that play a crucial role in the reproduction of seed plants. Understanding why pollen is well-preserved as a fossil is essential for understanding the geological history and plant evolution.
The pollen grains are composed of two main layers: the exine and the intine. Let's discuss these layers and why the exine is crucial for preserving pollen grains as fossils:
Thus, the correct answer to why pollen grains remain preserved as fossils is due to the exine layer.
| Pair of skeletal parts | Category | |
|---|---|---|
| (a)$\,\,$ | Sternum and ribs$\,\,$ | Axial skeleton |
| (b)$\,\,$ | Clavicle and glenoid cavity$\,\,$ | Pelvic girdle |
| (c)$\,\,$ | Flumerus and ulna$\,\,$ | Appendicular skeleton |
| (d)$\,\,$ | Malleus and stapes$\,\,$ | Ear ossicles |