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  4. The flower garden banks Siderastrea siderea coral as a candidate global boundary stratotype section and point for the Anthropocene series
 
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The flower garden banks Siderastrea siderea coral as a candidate global boundary stratotype section and point for the Anthropocene series

Journal
Anthropocene Review
Date Issued
2023-01-01
Author(s)
DeLong, Kristine L.
Palmer, Kylie
Wagner, Amy J.
Weerabaddana, Mudith M.
Slowey, Niall
Herrmann, Achim D.
Duprey, Nicolas
Martínez-García, Alfredo
Jung, Jonathan
Hajdas, Irka
Rose, Neil L.
Roberts, Sarah L.
Roberts, Lucy R.
Cundy, Andrew B.
Gaca, Pawel
Andrew Milton, J.
Yang, Handong
Turner, Simon D.
Huang, Chun Yuan
CHUAN-CHOU SHEN  
Zinke, Jens
DOI
10.1177/20530196221147616
URI
https://scholars.lib.ntu.edu.tw/handle/123456789/629932
URL
https://api.elsevier.com/content/abstract/scopus_id/85147570602
Abstract
The proposed Anthropocene Global Boundary Stratotype Section and Point (GSSP) candidate site of West Flower Garden Bank (27.8762°N, 93.8147°W) is an open ocean location in the Gulf of Mexico with a submerged coral reef and few direct human impacts. Corals contain highly accurate and precise (<±1 year) internal chronologies, similar to tree rings, and their exoskeletons are formed of aragonite and can be preserved in the rock record. Here we present results from a large Siderastrea siderea coral (core 05WFGB3; 1755–2005 CE) sampled with annual and monthly resolutions that show clear markers of global and regional human impacts. Atmospheric nuclear bomb testing by-products (14C, 239+240Pu) have clear increases in this coral starting in 1957 for 14C and the first increase in 1956 for 239+240Pu (potential bases for the Anthropocene GSSP). Coral δ13C declined especially after 1956 consistent with the Suess Effect resulting from the burning of fossil fuels. Coral skeletal δ15N starts to increase in 1963 corresponding with the increase in agricultural fertilizers. Coral Hg concentrations (1933–1980) loosely track fluctuations in industrial pollution and coral Ba/Ca increases from 1965–1983 when offshore oil operations expand after 1947. Coral temperature proxies contain the 20th-century global warming trend whereas coral growth declines during this interval.
Subjects
Ba/Ca | carbon isotopes | mercury | nitrogen isotopes | oxygen isotopes | plutonium | radiocarbon | Sr/Ca
SDGs

[SDGs]SDG13

[SDGs]SDG14

Publisher
SAGE PUBLICATIONS INC
Type
journal article

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