Non-linear effects in the determination of paleotemperature U37k′ alkenone ratios by chemical ionization mass spectrometry

被引:8
作者
Chaler, R [1 ]
Villanueva, J [1 ]
Grimalt, JO [1 ]
机构
[1] CSIC, ICER, ES-08034 Barcelona, Catalonia, Spain
关键词
paleotemperature; geochemistry; U-37(k ') index; alkenones; ketones;
D O I
10.1016/S0021-9673(03)01188-9
中图分类号
Q5 [生物化学];
学科分类号
071010 ; 081704 ;
摘要
The performance of gas chromatography coupled to mass spectrometry in the positive chemical ionization mode using ammonia as reagent gas (GC-PCI-MS) in the analysis of C-37 alkenones for paleotemperature estimation has been U-37(k') re-evaluated. In some conditions, the discrepancies observed in the measurement of the 37 index with this technique as compared with GC equipped with flame ionization detection (GC-FID) cannot be explained by differences in sensitivity Uk(37)(k') between the tri- and diunsaturated alkenones. Thus, at low (currently <0.3) or high (currently >0.4) 37 values the GC-PCI-MS determinations may be observed to be lower or higher, respectively, than those measured with GC-FID. As shown by analysis of a series of synthetic C-37 alkenone standards these discrepant results can be explained by non linear effects in the GC-PCI-MS response factors. Second-order polynomial functions provide equations that describe better the signal to amount of analyte ratios. Users of GC-PCI-MS should calibrate their instruments with standards of known C-37 alkenone composition in order to minimize non-linear effects. (C) 2003 Elsevier B.V. All rights reserved.
引用
收藏
页码:87 / 93
页数:7
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