Richard S Vachula, Thomas M Cullen, Matthew R Galinger, J Conner Welch, Jeremiah Battaglia, Dallyn Smith, Matthew N Waters
{"title":"Morphometric characteristics of charcoal produced from plants native to the southeastern United States of America (USA)","authors":"Richard S Vachula, Thomas M Cullen, Matthew R Galinger, J Conner Welch, Jeremiah Battaglia, Dallyn Smith, Matthew N Waters","doi":"10.1177/09596836241274975","DOIUrl":null,"url":null,"abstract":"Charcoal shape variations provide insight into past fuel types burned, with charcoal length:width (L:W) being the most popular means of distinguishing fuel types. This paper presents morphometric data (L:W) of charcoal produced from plant taxa (n = 21) native to the southeastern United States of America (USA). These taxa included monocots (n = 3), dicots (n = 12), and gymnosperms (n = 6), which represented a range of growth habits including graminoids, trees, shrubs, and subshrubs. We further divided these taxa into tissues (n = 36 total samples) which included leaves, wood, bark, needles, stems, and a seed pod. Our results show that charcoal produced from plants native to southeastern USA exhibits more variable L:W values than those tested in previous research, but that when aggregated, they broadly agree with published L:W value ranges. Within the dicot group, leaves produced charcoal lower L:W values (median = 1.92, interquartile range (IQR) = 1.33) than wood (median = 2.43, IQR = 3.00), whereas the opposite was true for gymnosperms whose needles produced greater L:W values (median = 2.60, IQR = 3.22) than wood (median = 1.93, IQR = 1.44). The monocot graminoid we tested produced greater L:W values (median = 3.47, IQR = 6.02) than dicot or gymnosperm fuels. Further, our results provide conflicting perspectives on the likelihood of evolutionary relationships as the cause of variations in charcoal L:W values. Last, our results underscore the importance of site-specific experimental charcoal approaches to enable robust paleofire applications of charcoal morphometry.","PeriodicalId":517388,"journal":{"name":"The Holocene","volume":"10 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-08-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"The Holocene","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1177/09596836241274975","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Charcoal shape variations provide insight into past fuel types burned, with charcoal length:width (L:W) being the most popular means of distinguishing fuel types. This paper presents morphometric data (L:W) of charcoal produced from plant taxa (n = 21) native to the southeastern United States of America (USA). These taxa included monocots (n = 3), dicots (n = 12), and gymnosperms (n = 6), which represented a range of growth habits including graminoids, trees, shrubs, and subshrubs. We further divided these taxa into tissues (n = 36 total samples) which included leaves, wood, bark, needles, stems, and a seed pod. Our results show that charcoal produced from plants native to southeastern USA exhibits more variable L:W values than those tested in previous research, but that when aggregated, they broadly agree with published L:W value ranges. Within the dicot group, leaves produced charcoal lower L:W values (median = 1.92, interquartile range (IQR) = 1.33) than wood (median = 2.43, IQR = 3.00), whereas the opposite was true for gymnosperms whose needles produced greater L:W values (median = 2.60, IQR = 3.22) than wood (median = 1.93, IQR = 1.44). The monocot graminoid we tested produced greater L:W values (median = 3.47, IQR = 6.02) than dicot or gymnosperm fuels. Further, our results provide conflicting perspectives on the likelihood of evolutionary relationships as the cause of variations in charcoal L:W values. Last, our results underscore the importance of site-specific experimental charcoal approaches to enable robust paleofire applications of charcoal morphometry.