Climate Change Data Portal
DOI | 10.1016/j.palaeo.2019.03.010 |
Sedimentary pyrite framboid size-frequency distributions: A meta-analysis | |
Rickard D. | |
发表日期 | 2019 |
ISSN | 0031-0182 |
起始页码 | 62 |
结束页码 | 75 |
卷号 | 522 |
英文摘要 | Framboids, microscopic sub-spheroidal aggregates of pyrite microcrystals, are found in sediments of all ages and framboid size-frequency distributions are widely used to determine the oxygenation states of paleo-waters. Sedimentary framboid populations display unimodal log-normal size distributions as a consequence of the multiplicative central limit theorem in probability theory. The application of additive statistics to framboid populations and their consequent characterization in terms of arithmetic means and standard deviations is wrong because it predicts a subset of framboids with negative diameters. A meta–analysis of 377 sets of measurements of the diameters of 48,063 pyrite framboids from 104 sediment and sedimentary rock locations shows that the geometric mean diameter of sedimentary framboids is 6.2 μm and the geometric standard deviation is 1.5. Ninety-five percent of all sedimentary framboids have geometric mean diameters between 2.9 and 13.9 μm. The geometric mean diameter of modern syngenetic framboids formed within euxinic water columns is 4.7 μm and that of diagenetic framboids formed within sediments is 6.7 μm. The estimated measurement error is ±10%. Framboid mean diameters can be used to help discriminate the oxygenation state of paleo-waters. A minimum number of 30 measurements is required and ideally ≥100 measurements are recommended. The conflicting evidence reported in the literature for the application of framboid size-frequency measurements results mainly from the intrinsic nature of statistical analyses: there is always a finite chance that a particular framboid size-frequency distribution is a result of either syngenetic or diagenetic processes. Including the systematic stereological error in framboid size measurements, the geometric mean size range for syngenetic framboids is 2.9–10.9 μm and that for diagenetic framboids 3.1–20.9 μm. This suggests a significant overlap in geometric mean diameters of framboids from euxinic and non-euxinic environments between ~3 and ~11 μm. Geometric mean framboid diameters within this size range are not robust proxies for paleo-water oxygenation conditions. The origin of the smaller sizes of syngenetic compared with diagenetic framboids appears to be related to the limited time available for framboid crystal growth within the water column. The statistical uncertainty in assigning particular framboid size-frequency distributions to defined oxygenation conditions results mainly from (a) some diagenetic framboids forming over a limited time, thereby also producing smaller framboids and (b) mixtures of syngenetic and diagenetic framboid populations through unavoidable time-averaging of samples. The absence of any significant differences in the sizes of modern and ancient framboids indicates that framboids do not continue to grow over extended time periods: once formed they remain the same over geologic time periods and only change through infilling, overgrowth and recrystallization. The result is that ancient framboids may sample the contemporary paleoenvironment in the sedimentary system in which they are found. © 2019 |
英文关键词 | Framboid; Paleoenvironment; Pyrite; Sediment; Size |
语种 | 英语 |
scopus关键词 | diagenesis; euxinic environment; geometry; micromorphology; oxygenation; paleoenvironment; pyrite; sedimentary rock; size distribution |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/150998 |
作者单位 | School of Earth and Ocean Sciences, Cardiff University, Cardiff, CF10 3AT, United Kingdom |
推荐引用方式 GB/T 7714 | Rickard D.. Sedimentary pyrite framboid size-frequency distributions: A meta-analysis[J],2019,522. |
APA | Rickard D..(2019).Sedimentary pyrite framboid size-frequency distributions: A meta-analysis.Palaeogeography, Palaeoclimatology, Palaeoecology,522. |
MLA | Rickard D.."Sedimentary pyrite framboid size-frequency distributions: A meta-analysis".Palaeogeography, Palaeoclimatology, Palaeoecology 522(2019). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Rickard D.]的文章 |
百度学术 |
百度学术中相似的文章 |
[Rickard D.]的文章 |
必应学术 |
必应学术中相似的文章 |
[Rickard D.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。