作者: P Kiran Kumar , Shraddha T Band , R Ramesh , Neeraj Awasthi , None
DOI: 10.1016/J.QUAINT.2018.03.025
关键词: Foraminifera 、 Globorotalia menardii 、 Last Glacial Maximum 、 Geology 、 Globigerinoides 、 Oceanography 、 δ18O 、 Stratification (water) 、 Holocene 、 Monsoon
摘要: Abstract Using new oxygen isotope (δ18O) data of three planktonic foraminiferal (Globigerinoides ruber, Globigerinoides sacculifer and Globorotalia menardii) species from a sediment core SK-234-60, collected the Andaman Sea, we infer that summer monsoon was weaker during Marine Isotopic Stage-3 (MIS-3) than early Holocene but stronger MIS-2. Further, an abrupt decrease in mid-Holocene between ∼7 4.5 ka is observed. The difference δ18O with different habitats depth also enables reconstruction past ocean stratification over Sea. Distinct weak strong freshwater-induced upper stratifications are observed last ∼66 ka. A Last Glacial Maximum (LGM) This due to prevailing positive negative Evaporation minus Precipitation (E-P) conditions, respectively. Weaker ∼32 mid-MIS-3 observed, whereas ∼42-39 Stronger associated higher seen ∼62 Likewise, Heinrich events stratification.