海洋地质与第四纪地质2026，Vol.46Issue(3)：163-176,14.DOI:10.16562/j.cnki.0256-1492.2025102401
西北印度洋中脊侧翼MIS 2期和MIS 1期洋底氧化还原环境与底层水组成对比分析
Relationship between redox condition and bottom water composition in the Mid-Ocean Ridge flank of the Northwest Indian Ocean during MIS 2 and MIS 1
摘要
Abstract
Deep-water circulation in the Indian Ocean plays a vital role in global oceanic processes,and the bottom water was derived primarily from the Antarctic Bottom Water(AABW)and North Atlantic Deep Water(NADW).We systematically investigated the evolution of bottom-water redox conditions and water mass composition during glacial-interglacial cycles,for which the Nd isotopes in the ferromanganese oxide phases and redox-sensitive elements in sediment cores from both sides of the Northwest Indian Ocean Ridge were analyzed in consideration of available data of MIS 1(Marine Isotope Stage 1).The enrichment factors(EF)of sensitive elements such as U and V(UEF,VEF＜2),and extremely low U/Th ratios suggested that the study area was remained in an overall oxic condition since the MIS 2(Marine Isotope Stage 2).The εNd values of the authigenic Fe-Mn oxide phase sediments ranged from-6.56 to-6.83 in MIS 2 stage,while those in MIS 1 stage were from-7.16 to-8.09.The binary mixing model calculations showed that the bottom water was consistently dominated by Antarctic Bottom Water(AABW)during both MIS 2 and MIS 1(accounting for＞75%).Although εNd values show a slightly negative shift after entering the interglacial period due to the variation of the source area characteristics,the difference in εNd value between glacial and interglacial stages stems mainly from the changes in the water mass end-members themselves,rather than from variations in regional water mass mixing proportions.The notable isotopic consistency on both sides of the ridge reflects efficient ventilation of the bottom water in the Northwest Indian Ocean with Circumpolar Deep Water(CDW)from the southern main passageway,occurring equally on both sides of the ridge.关键词
氧化还原敏感元素/Nd同位素/南极底层水/冰期—间冰期变化/西北印度洋Key words
redox-sensitive elements/Nd isotope/Antarctic Bottom water/glacial-interglacial changes/Northwest Indian Ocean分类
海洋科学引用本文复制引用
邓浪,金丽娜,乔淑卿,李小艳,陈亮,殷征欣..西北印度洋中脊侧翼MIS 2期和MIS 1期洋底氧化还原环境与底层水组成对比分析[J].海洋地质与第四纪地质,2026,46(3):163-176,14.基金项目
国家自然科学基金"MIS7期以来热带西印度洋底层水演化及其环境气候效应"(42376083),"中印度洋脊侧翼断裂带内钙质浊流沉积过程及其对地震活动的响应"(42206072) （42376083）
科技部国家重点研发项目"晚新生代亚洲大陆风化过程、沉积记录及碳汇效应"(2022YFF0800503) （2022YFF0800503）
