Utility of salt-marsh foraminifera, testate amoebae and bulk-sediment δ¹³C values as sea-level indicators in Newfoundland, Canada

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• 作者：Andrew C. Kemp^a ; ^{andrew.kemp@tufts.edu} ; Alexander J. Wright^b ; Robert L. Barnett^c ; ^e ; Andrea D. Hawkes^d ; Dan J. Charman^e ; Colby Sameshima^a ; Alexandra N. King^d ; Hailey C. Mooney^d ; Robin J. Edwards^f ; Benjamin P. Horton^g ; ^h ; Orson van de Plassche^b
• 刊名：Marine Micropaleontology
• 出版年：2017
• 出版时间：January 2017
• 年：2017
• 卷：130
• 期：Complete
• 页码：43-59
• 全文大小：1561 K
• 卷排序：130

文摘

Foraminifera are sea-level indicators, but high-marsh assemblages vary among sites. Testate amoebae assemblages are likely affected by preservation bias. Sediment δ13C values cannot distinguish between salt-marsh and freshwater samples. We produce 3 Holocene sea-level index points using a simple, multi-proxy approach.