Passage
When Dr. Julian Thorne first looked at the ice core sample recovered from the Amundsen Sea, he was searching for the telltale ash layers of the 1815 Tambora eruption. However, the unexpected presence of micro-particles of cobalt at the deeper three-hundred-meter mark shifted his focus entirely. This depth corresponded to a period long before industrialization, suggesting an ancient cosmic impact event. To verify this, Julian sent an aliquot of the melted ice to the mass spectrometry lab in Denver. He had only been permitted to access these rare cores after securing the highly competitive polar research fellowship the previous autumn. Now, as he waited for the spectral readouts, Julian pulled up the digitized logbooks of the HMS Challenger from the late nineteenth century. Those early oceanographers had recorded strange, metallic sediment in their dredge buckets, a detail Julian had dismissed as contamination when he first read their reports during his graduate studies. The Denver lab’s automated notification chimed, interrupting his thoughts; the isotopic ratio of the cobalt was indeed non-terrestrial.
Based on the implicit chronological cues in the passage, arrange the following events in the order in which they occurred, from earliest to latest.
- 1Oceanographers on the HMS Challenger record metallic sediment in dredge buckets.
- 2Julian reads the HMS Challenger logbooks and dismisses the sediment records as contamination.
- 3Julian secures a polar research fellowship that grants him access to ice cores.
- 4Julian sends a portion of the melted ice core sample to a laboratory in Denver.