Mg and Sr uptake in benthic foraminifera Ammonia aomoriensis based on culture and field studies | |
Yu, Zhoufei1,3; Lei, Yanli1,6,7; Li, Tiegang2,4; Zhang, Shuai5; Xiong, Zhifang2,4 | |
刊名 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY |
2019-04-15 | |
卷号 | 520页码:229-239 |
关键词 | Ammonia beccarii Interspecific difference Biological control Temperature Salinity |
ISSN号 | 0031-0182 |
DOI | 10.1016/j.palaeo.2019.02.001 |
英文摘要 | Trace elements incorporated in foraminiferal test are commonly used as paleoproxies, however, the incorporation of trace elements is controlled by more than one environmental parameter. We conducted one year sampling from June 2014 to May 2015 in the Qingdao intertidal flat, the Yellow Sea, and retrieved surface samples in the Jiaozhou Bay (3.9-6.8 m water depth), the Yellow Sea in February 2015, as well as performed a laboratory culture experiment under temperature 6-24 degrees C and salinity 24-33 psu, by combining delta O-18(c) values of field A. aomoriensis, parameters controlling Mg/Ca and Sr/Ca ratios of Ammonia aomoriensis were investigated. Under constant seawater chemistry, temperature dominates the magnesium incorporation into A. aomoriensis test by an exponential increase of 5.1% per degrees C (Mg/Ca = 1.0980 ( +/- 0.2073) e(0.0510 (+/- 0.0097) T); Mg/Ca = 0.5565 ( +/- 0.3897) + 0.1279 ( +/- 0.0242) T, 2.4-24 degrees C including field samples). Whereas, temperature has no significant effect on Strontium uptake. Calcite Sr/Ca of A. aomoriensis is primarily explained by Mg/Ca value (similar to 3% per mmol/mol). Salinity variations are of subordinate importance for both Mg and Sr content in the test of A. aomoriensis, Mg/Ca raises linearly with approximately 2% per salinity unit, and Sr/Ca increases similar to 1% per salinity unit. Importantly, biological mechanism might be an inestimable factor perturbing Mg and Sr response to environmental parameters in natural waters, complicating the paleoclimate reconstruction. |
资助项目 | Continental Shelf Drilling Program of China[GZH201100202] |
WOS关键词 | CARBONATE ION CONCENTRATION ; MG/CA-TEMPERATURE ; SR/CA RATIOS ; PLANKTONIC-FORAMINIFERA ; GLOBIGERINOIDES-RUBER ; ISOTOPE FRACTIONATION ; CLEANING PROCEDURES ; WATER TEMPERATURE ; STABLE-ISOTOPE ; SALINITY |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
语种 | 英语 |
出版者 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:000463125100019 |
内容类型 | 期刊论文 |
源URL | [http://ir.fio.com.cn:8080/handle/2SI8HI0U/24765] |
专题 | 自然资源部第一海洋研究所 |
通讯作者 | Lei, Yanli; Li, Tiegang |
作者单位 | 1.Chinese Acad Sci, Lab Marine Organism Taxon & Phylogeny, Inst Oceanol, Qingdao 266071, Shandong, Peoples R China 2.MNR, Key Lab Marine Sedimentol & Environm Geol, Inst Oceanog 1, Qingdao 266061, Shandong, Peoples R China 3.Chinese Acad Sci, CAS Key Lab Econ Stratig & Palaeogeog, Nanjing Inst Geol & Palaeontol, Ctr Excellence Life & Paleoenvironm, Nanjing 210008, Jiangsu, Peoples R China 4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Shandong, Peoples R China 5.Hohai Univ, Nanjing 210098, Jiangsu, Peoples R China 6.Univ Chinese Acad Sci, Beijing, Peoples R China 7.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Shandong, Peoples R China |
推荐引用方式 GB/T 7714 | Yu, Zhoufei,Lei, Yanli,Li, Tiegang,et al. Mg and Sr uptake in benthic foraminifera Ammonia aomoriensis based on culture and field studies[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2019,520:229-239. |
APA | Yu, Zhoufei,Lei, Yanli,Li, Tiegang,Zhang, Shuai,&Xiong, Zhifang.(2019).Mg and Sr uptake in benthic foraminifera Ammonia aomoriensis based on culture and field studies.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,520,229-239. |
MLA | Yu, Zhoufei,et al."Mg and Sr uptake in benthic foraminifera Ammonia aomoriensis based on culture and field studies".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 520(2019):229-239. |
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