How can a geological time scale best be reconstructed? a) comparing vestigial structures in living species . b) comparing homologous structures in living species. c) examining homologous structures in fossil remains. d) examining the written records of scientist from past structures.

C.

This makes the most sense to me. Studying fossils is how it is usually done. Many things can be told from this.

the transfer for conduction is the heat transfering from the liquid to the spoon

the transfer for convection is the heat rising from the liquid to the air

the transfer for radiation is the heat going through the sides of the cup and to the air

at least that is what i would do

glycolysis is a process that fuel your metabolism. it is apart of cellular respiration the process that produce atp.