Question:

Which of the following microfossils has/have a geological range from Cambrian to Recent?

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Diatoms and dinoflagellates evolved much later than the Cambrian; only two of the four groups go back that far.
Updated On: Jul 20, 2026
  • Foraminifera
  • Diatoms
  • Radiolaria
  • Dinoflagellates
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The Correct Option is A, C

Solution and Explanation

Step 1: Understanding the Question.
The question asks which of the four microfossil groups have existed continuously from the Cambrian period right up to the present day, that is, which groups have the longest, essentially unbroken, geological ranges.

Step 2: Key Concept.
Different microfossil groups originated at different times in Earth's history, and their first appearance in the fossil record sets the start of their geological range. Groups that evolved early, in the Cambrian, and have living representatives today are said to range Cambrian to Recent. Groups that evolved later only range from their time of first appearance to the present.

Step 3: Detailed Explanation.

(A) Foraminifera: These shelled protists first appear in the Cambrian and have living representatives in modern oceans, so their range is Cambrian to Recent.

(B) Diatoms: These are single-celled algae with silica frustules, but they first appear in the fossil record in the Jurassic period, much later than the Cambrian, and continue to the present, so their range is Jurassic to Recent, not Cambrian to Recent.

(C) Radiolaria: These are amoeboid protozoa with silica skeletons, and like foraminifera, they have a long fossil record extending back to the Cambrian, with living forms still present in the oceans today, so their range is Cambrian to Recent.

(D) Dinoflagellates: These are flagellate algae whose reliable cyst fossil record begins in the Triassic period, well after the Cambrian, and continues to the present, so their range is Triassic to Recent, not Cambrian to Recent.

Step 4: Final Answer.
Foraminifera and Radiolaria are the two microfossil groups with a continuous fossil record from the Cambrian to the present, while diatoms and dinoflagellates appear much later in the geological record.
\[ \boxed{\text{Foraminifera and Radiolaria}} \]
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