What are biological clocks?
What are biological clocks?
Biological clocks are an organism’s innate timing device. They’re composed of specific molecules (proteins) that interact in cells throughout the body. Biological clocks are found in nearly every tissue and organ. Researchers have identified similar genes in people, fruit flies, mice, fungi, and several Credit: NIGMS.
Why is it important to synchronize your biological clock with schedule?
By synchronizing your biological clock with your daily schedule, you can make the most of your day and feel more accomplished and motivated. Circadian rhythms affect your sleep-wake cycle, eating habits, body temperature, digestion, hormone levels, and other body functions.
Is your biological clock at odds with your schedule?
Some people tend to experience energy peaks earlier in the day, while others are more active during the later hours. Thanks to the demands of daily life, it may sometimes feel like your biological clock and schedule are at odds. So what can you do if your daily schedule is out of sync with your biological clock?
How can I keep my biological clock on track?
One way to keep your biological clock on track is to maintain a consistent sleep schedule. Try to go to bed and wake up at the same time every day, even on the weekends. You want your body to get used to a routine. When you do this, you support a healthy circadian clock.
What does a Cryptomeria tree look like?
Cryptomeria is a very large evergreen tree, reaching up to 70 m (230 ft) tall and 4 m (13 ft) trunk diameter, with red-brown bark which peels in vertical strips. The leaves are arranged spirally, needle-like, 0.5–1 cm ( 1⁄4 – 3⁄8 in) long; and the seed cones globular, 1–2 cm ( 1⁄2 – 3⁄4 in) diameter with about 20–40 scales.
What is the scientific name of Cryptomeria?
Cryptomeria (literally “hidden parts”) is a monotypic genus of conifer in the cypress family Cupressaceae, formerly belonging to the family Taxodiaceae.
Where did Cryptomeria japonica come from?
Cryptomeria japonica was described from the Late Miocene of Georgia and from the Pliocene of Duab, Abkhazia. It has also been described from the Pliocene of Honshu, Japan, Late Pliocene of Osaka, Japan and from the Pleistocene of Kyushu, Japan.
