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It can be inferred from the passage that in sediment cores from the North Atlantic`s deep waters, the portions that correspond to the Little Ice Age
  • Adiffer very little in composition from the portions that correspond to the Medieval Warm Period
  • Bfluctuate significantly in composition between the portions corresponding to the 1300s and the portions corresponding to the 1700s
  • Cwould be likely to contain a proportion of red-stained grains closer to 17 percent than to 5 percent.
  • Dshow a much higher proportion of red-stained grains in cores extracted from the far north of the North Atlantic than in cores extracted from further south.
  • Ewere formed in part as a result of Gulf Stream waters having been pulled northward

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