冰期至间冰期的气候漂移驱动了大陆风化作用的变化，这种变化改变了铁、硅和营养物质的风成的及河流的向海输入量，同时造成较高的冰期大洋生物生产力、较低的底层水含氧量、增长的有机碳埋藏速率和沉积物的氧化还原反应速率以及较低的大气二氧化碳。然而，以下因素限制了... Climate shifts from the Ice Age to the interglacials have driven changes in continental weathering that have changed the abundance of iron, silicon, and nutrients into the sea and the river’s input to the sea, resulting in higher glacial marine bioproductivity, lower The underlying water oxygen content, increased organic carbon burial rate and sediment redox reaction rates, as well as lower atmospheric carbon dioxide. However, the following factors limit ...