Nature Communications (Jan 2022)
Abrupt conclusion of the late Miocene-early Pliocene biogenic bloom at 4.6-4.4 Ma
Abstract
What caused the end of the high ocean productivity in the tropics in late Miocene-early Pliocene is debated. Here, deep-sea sediment records reveal that productivity abruptly declined 4.6 million years ago, potentially linked to reduced seasonality and monsoon intensity that led to decreased nutrient supply to the oceans.