Study of sclerochronology by laser ablation ICP-MS
Study of sclerochronology by laser ablation ICP-MS
复制标题
通过激光烧蚀 ICP-MS 进行硬化年代学研究
DOI:
10.1039/b002014l
复制
发表时间:
2000
期刊:
影响因子:
--
通讯作者:
M. Leng
中科院分区:
文献类型:
--
作者:
H. Toland;Bill Perkins;N. Pearce;Fergus Keenan;M. Leng
Sclerochronology is to shells what dendrochronology is to trees, i.e., growth structures within some shells (in this case the bivalve mollusc Arctica islandica L., the Ocean Quahoc) resemble, in form and content, those growth structures in trees, which grow with an annual periodicity. By utilising laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS), allied with stable isotope analysis to sample the growth structures within shells, environmental conditions (e.g., ambient temperature, salinity, seasonality and productivity) prevalent at the time of shell genesis may be ascertained. A limiting factor in the retrieval of any data from biogenic carbonates such as these is the size of the repeated growth structures from which to extract information. In the case of Arctica, these can be as low as tens of µm. Micro-drilling techniques, such as those commonly used in isotope analyses, are constrained by the size of the drill bit used to collect the sample. LA-ICP-MS, with its ultra-high spatial resolution (10–20 µm ablation pits) and precision, delivers highly constrained analysis allowing accurate multi-element sampling of seasonal growth bands within shells. It may be feasible to use the elements strontium, magnesium and barium as records of inter-annual environmental conditions, thus removing the need to carry out stable isotope analyses in some instances, particularly where the size of the material to be sampled demands the high resolution of LA-ICP-MS.