What produced the platinum spike in the GISP2 ice core near the Younger Dryas onset?
Four answers, none aheadNone is ahead yet. See what would settle it.
Where it stands
Four answers have been proposed. None is ahead on the evidence yet. Four are still possible.
Answers 4
History
- Petaev et al. puts forward: an iridium-poor, highly differentiated iron meteorite.
- Petaev et al.: superchondritic Pt/Al and fractionated Pt/Ir ratios exclude mantle and chondritic sources.For: An iridium-poor, highly differentiated iron meteorite.
- Reinig et al.: the eruption is dated about 130 years before the onset.Against: The Laacher See eruption.
- Green et al. puts forward: fractionated gas condensates from an unidentified volcanic eruption, probably an Icelandic subglacial or…
- Green et al. puts forward: the Laacher See eruption.
- Green et al.: the spike spans about 14 years.Against: An iridium-poor, highly differentiated iron meteorite.
- Green et al.: no eruption has been identified for the interval.Against: Fractionated gas condensates from an unidentified volcanic eruption, probably an Icelandic subglacial or…
- Green et al.: platinum-group patterns in submarine volcanic gas condensates (Niuatahi-Motutahi, Tonga) resemble the spike.For: Fractionated gas condensates from an unidentified volcanic eruption, probably an Icelandic subglacial or…
- Green et al.: new platinum and iridium data from the tephra do not match the spike.Against: The Laacher See eruption.
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