Biomarkers, molecular fossils, are organic compounds in Holocene to Pr
ecambrian sedimentary deposits that can be related to specific chemica
l compounds produced in the biosphere. We demonstrate here that 24-nor
cholestane biomarkers, i.e., C26 steranes (saturated hydrocarbons havi
ng a steroid skeleton), can be useful to constrain the age and paleola
titude of geologic samples. The biological precursors of 24-norcholest
anes remain unclear, but samples from more than 100 basins provide evi
dence that 24-norcholestanes may be derived directly or indirectly fro
m diatoms, Ratios of 24-norcholestanes to 27-norcholestanes show an in
itial increase above background in Jurassic oils, but they increase dr
amatically in Cretaceous oils, coincident with diatom evolution. The h
ighest ratios are found in oils and rock extracts from Oligocene or yo
unger marine siliceous source rocks in which the sources were deposite
d at paleolatitudes greater than 30 degrees N.