Now chemists and geologists from Binghamton University and Johns Hopkins University have found proof of shifting ocean chemistry in ancient salt deposits. 現在丙罕頓大學(xué)與約翰霍普金斯大學(xué)的化學(xué)家與地質(zhì)學(xué)家，在古代鹽沉積層中發(fā)現了海洋化學(xué)會(huì )變動(dòng)的證據。
Abyssal benthic barite, as a reliable proxy of paleoclimate, is widely used for reconstruction of Cenozoic marine chemistry properties and paleoproductivity. 摘要深海沉積成因重晶石作為重要的古海洋環(huán)境指示物，被廣泛應用于新生代海洋化學(xué)和古生產(chǎn)力的重建，成為全球變化研究的重要分析對象之一。
