Paleoclimatologists analyzing polar ice cores have established the following:
• Every polar ice core segment that exhibits an anomalous sulfate spike without an accompanying basaltic cryptotephra deposit was formed during a period of non-explosive effusive volcanism.
• In the Amundsen-Scott ice core, every segment corresponding to the mid-Holocene climatic anomaly contains either a basaltic cryptotephra deposit or a high concentration of micro-meteoritic iridium, but not both.
• No polar ice core segment containing a high concentration of micro-meteoritic iridium was formed during a period of non-explosive effusive volcanism.
• Sample AS-442 is a segment from the Amundsen-Scott ice core that corresponds to the mid-Holocene climatic anomaly and exhibits an anomalous sulfate spike.
If the statements above are true, which one of the following must be true?
- ASample AS-442 was formed during a period of non-explosive effusive volcanism.
- BAny polar ice core segment formed during a period of non-explosive effusive volcanism exhibits an anomalous sulfate spike.
- Sample AS-442 contains a basaltic cryptotephra deposit.Cevap
- DEvery segment in the Amundsen-Scott ice core that exhibits an anomalous sulfate spike corresponds to the mid-Holocene climatic anomaly.
- EHigh concentrations of micro-meteoritic iridium in polar ice cores are caused exclusively by explosive volcanic eruptions.