Decoding nonlinear growth rates in biogenic environmental archives -: art. no. Q12015

被引:20
作者
De Ridder, F
Pintelon, R
Schoukens, J
Gillikin, D
André, L
Baeyens, W
de Brauwere, A
Dehairs, F
机构
[1] Free Univ Brussels, Dept Elect & Instrumentat, B-1050 Brussels, Belgium
[2] Free Univ Brussels, Dept Analyt & Environm Chem, B-1050 Brussels, Belgium
[3] Royal Museum Cent Africa, Sect Petrog Mineral Geochem, B-3080 Tervuren, Belgium
关键词
growth and accretion rate; time base distortion; stable isotopes; carbonate; environmental proxies; paleoclimate; mathematical geophysics : modeling; oceanography : biological and chemical : stable isotopes; oceanography : biological and chemical : trace elements;
D O I
10.1029/2004GC000771
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The record of an environmental proxy along a growth axis in biogenic carbonates can reflect changing environmental conditions experienced during the lifetime of the organism. When a chronology of the growth axis is not available, a method based on anchor points is commonly used to introduce a time grid. Between these anchor points a constant growth rate is generally assumed, despite the fact that growth rates change during life in most organisms. Here, we present a method which refines the constant growth rate assumption, at least in situations where the environmental proxy has a periodic component in its signal. A nonlinear growth rate can then be estimated, enabling the construction of a more realistic time base. The anchor point method and the method proposed here are first compared on a synthetic record. It is shown that the choice of the anchor points, which is always a subjective one, is largely influenced by the stochastic noise on the data record. This results in biased growth rate profiles and biased time grids. Next we apply the method on the Mg record in the bivalve Isognomon ephippium, on three samples of the clam Saxidomus giganteus from Washington State and on the Vanuatu coral stable isotope record. The method developed is applicable to a wide range of proxy records, which are measured along an indirect time grid and are complicated by nonlinear accretion rates. Furthermore, this method which takes variable growth rates into account opens perspectives on quantitative modeling of the relationship between environmental proxies recorded by accretive archives and the instrumental record, like temperature or salinity.
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页数:16
相关论文
共 26 条
[1]   Corals at their latitudinal limits:: laser ablation trace element systematics in Porites from Shirigai Bay, Japan [J].
Fallon, SJ ;
McCulloch, MT ;
van Woesik, R ;
Sinclair, DJ .
EARTH AND PLANETARY SCIENCE LETTERS, 1999, 172 (3-4) :221-238
[2]   Trace element variation in speleothem aragonite: potential for palaeoenvironmental reconstruction [J].
Finch, AA ;
Shaw, PA ;
Weedon, GP ;
Holmgren, K .
EARTH AND PLANETARY SCIENCE LETTERS, 2001, 186 (02) :255-267
[3]  
GILLIKIN DP, 2004, IN PRESS PALAEOGEOGR
[4]  
HERBERT TD, 1994, SPEC PUBL INT ASS SE, V19, P483
[5]  
JONES DS, 1983, AM SCI, V71, P384
[6]  
Klein RT, 1996, GEOLOGY, V24, P415, DOI 10.1130/0091-7613(1996)024<0415:BSRSST>2.3.CO
[7]  
2
[8]   Sea-surface temperature variability in the 16th century at Bermuda inferred from coral records [J].
Kuhnert, H ;
Pätzold, J ;
Schnetger, B ;
Wefer, G .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2002, 179 (3-4) :159-171
[9]  
Lazareth CE, 2000, GEOLOGY, V28, P515
[10]  
LAZARETH CE, 2003, ESTUAR COAST SHELF S, V56, P1