安达曼海浮游有孔虫群落对全新世海洋环境变化的响应

doi:10.11978/2019010

Abstract

Abstract:

Through analysis of planktonic foraminifera in a gravity core ADM-C1 from the Andaman Sea, the response of planktonic foraminifera to Holocene marine environmental changes in the sea was discussed. The result shows that the planktonic foraminiferal communities in this region are dominated by tropical warm-water species Globigerinoides ruber, Globigerinoides sacculifer, Neogloboquadrina dutertrei, and Pulleniatina obliquiloculata. The relative abundance of G. ruber shows a gradual decreased trend from the early Holocene to present, which is roughly opposite to that of G. sacculifer. The relative abundance of N. dutertrei is higher during 11 to 7.9 ka BP (before present), generally lower during 7.9 to 3.8 ka BP, and then gradually increases after 3.8 ka BP. P. obliquiloculata shows an almost opposite trend to that of N. dutertrei. Our result indicates no obvious Pulleniatina Minimum Eventduring the late Holocene, occurs in the Andaman Sea. Q-mode factor analyses of planktonic foraminifera in the core ADM-C1 identify three stages in marine environmental changes during the Holocene. During the early Holocene (11-7.9 ka BP), planktonic foraminifera assemblage was dominated by G. ruber, N. dutertrei and G. bulloides, which reflected that strong summer monsoon and precipitation led to lower sea surface salinity, while the influence of winter monsoon was also strong during this stage. During 7.9-3.8 ka BP, G. ruber, P. obliquiloculata and Globigerinella aequilateralis dominated, indicating lower sea surface salinity during this period. Meanwhile, there was obviously increase in abundance of subsurface water species, reflecting strong mixing in the upper-ocean waters, possibly due to the strong Indian Ocean summer monsoon at this stage. After 3.8 ka BP, G. sacculifer, N. dutertrei and P. obliquiloculata became the dominant species. The abundance of G. ruber declined obviously, indicating that the salinity of surface sea water significantly increased during this period, which was consistent with the reduced Indian Ocean summer monsoon precipitation. The phase change of the Holocene marine environment reflected by the planktonic foraminiferal assemblages in the Andaman Sea is well consistent with the terrestrial records on the Indian Ocean summer monsoon, and it also shows good consistent with the wind intensity variation in Indian Ocean summer monsoon reflected by sensitive grain size proxy of the same core, suggesting rapid response of planktonic foraminifera to marine environmental changes in the tropical marginal seas.

Key words: Holocene, Andaman Sea, Planktonic foraminifera, Indian Ocean monsoon, Marine environment

ZHANG Lingzhi, XIANG Rong, TANG Linggang, YANG Yiping, ZHONG Fuchang. Response of planktonic foraminifera to Holocene marine environmental changes in the Andaman Sea[J].Journal of Tropical Oceanography, 2019, 38(6): 51-61.

Figures/Tables 7

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属种	主因子1	主因子2	主因子3
Globigerinoides ruber	2.943	0.466	-3.503
Globigerinoides sacculifer	-1.779	3.571	-0.606
Neogloboquadrina dutertrei	2.458	2.370	1.926
Pulleniatina obliquiloculata	-1.020	1.375	-1.210
Globorataloides hexagonus	0.176	-0.033	-0.202
Globigerinita glutinata	0.154	-0.015	-0.411
Globigerina bulloides	1.371	0.882	1.496
Globigerina calida	-0.110	-0.034	-0.389
Globiberinella aequilateralis	-0.953	0.443	-1.155
Globigerinoides tenellus	-0.145	0.020	-0.223
Globoquadrina conglomerata	-0.128	0.415	0.119
Globigerinoides conglobatus	-0.315	0.301	-0.201
Globorotalia menardii	-0.024	0.488	0.248
Globorotalia scitula	0.075	-0.021	0.040
Orbulina universa	-0.289	0.172	-0.271
Sphaeroidinella dehiscens	-0.072	0.131	0.009
Globorotalia tumida	0	0.035	0.028
Globorotalia ungulata	0.028	0.020	-0.001
Globorotalia theyeris	-0.004	-0.008	-0.042
Candeina nitida	-0.036	0.025	-0.039
Globigerina digitata	-0.011	0.012	-0.003
Globigerinella adamis	-0.011	0.012	-0.003
方差	36.253	28.209	34.714
累计方差	36.253	64.462	99.176

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Response of planktonic foraminifera to Holocene marine environmental changes in the Andaman Sea

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