Wiki User
β 8y agoApprox 6.1% remains.
Wiki User
β 6y agoThe answer depends on 3240 WHAT: seconds, days, years?
by multiplying the denominator with the whole number and adding the numerator. the denominator will remain the same.
1/4
The remainder is 2-p or 0.5p of the original amount.
This is true; if you multiply both numbers by the same number, the proportion will remain the same.
fossil
Probably it is dung that is a fossil
A hard and rock-like fossil is called a petrified fossil. Petrified fossils are formed when organic material is slowly replaced by minerals, turning the material into stone while preserving the original structure of the organism.
To calculate the fraction of atoms remaining in a fossil based on parent and daughter isotopes, you need to know the initial ratio of parent to daughter isotopes in the fossil and the current ratio. By comparing these ratios, you can determine the fraction of parent isotopes that have decayed into daughter isotopes, which indicates how much of the original parent isotopes remain in the fossil.
Fragmentation is a type of asexual reproduction that involves an organism starting to grow out of the parent organism that may or may not remain attached to the parent organism.
No, we just kind of guessed they were there. p.s. It would be the fossil remains, not fossils in remain.
Approx 1/8 will remain.
Plankton =
Homeostasis is the process by which living organisms regulate internal conditions to maintain stability, despite external changes. This involves mechanisms such as negative feedback loops to adjust physiological parameters within a narrow range conducive to optimal functioning. Various organ systems work together to monitor and adjust factors like temperature, pH, and nutrient levels to sustain homeostasis.
Yes. It came from an organism and is capable of decay.
When an organism is buried it is usually in sedementary rock, which is sof and layered. Over time the layers of sedements compact and can soak into the bones of an organism. As the bones are put under extreme pressure the become more like rocks and are thus presserved.
Stable