Holocene vegetation and wildfire disturbance in boreal central Yukon, Canada

IF 4.7 Q2 MATERIALS SCIENCE, BIOMATERIALS ACS Applied Bio Materials Pub Date : 2024-05-24 DOI:10.1139/as-2023-0070

K. Brown, P. Jain, Nicholas J.R. Hebda, Nicholas Conder, Richard J. Hebda, Les C. Cwynar

{"title":"Holocene vegetation and wildfire disturbance in boreal central Yukon, Canada","authors":"K. Brown, P. Jain, Nicholas J.R. Hebda, Nicholas Conder, Richard J. Hebda, Les C. Cwynar","doi":"10.1139/as-2023-0070","DOIUrl":null,"url":null,"abstract":"Sediment cores were collected from Wrong (WL) and Lenore (LL) lakes in boreal central Yukon Territory, Canada, spanning circa 6000 years. Analyses of pollen, charcoal, magnetic susceptibility, levoglucosan, and down-scaled paleoclimatic data reveal the vegetation history and character/drivers of Holocene fire disturbance. Boreal forest has persisted in the region for millennia, with a regional mid-Holocene expansion of Picea mariana followed by expansion of Pinus contorta in the latest Holocene. The shortest reconstructed fire return intervals (FRI; ca. 110-125 years) occurred in the mid-Holocene, coincident with the development of highly flammable Picea-dominated forest and warm, dry summers that were characterized by elevated JJA Z500 anomalies and associated with an eastward/intense Aleutian Low. In the late-Holocene, FRI increased to ca. 240 years at WL and 280 years LL. Drivers of this change include regional cooling and increased precipitation, with a westward/weaker Aleutian Low position delivering more moisture to interior Yukon. Longer FRIs allowed for greater fuel accumulation between fires, enhancing fire size/severity. While higher fire frequency is noted in the mid-Holocene and increased fire size/severity in the late-Holocene, recent changes in Yukon fire disturbance suggest that the fire regime may soon lie outside the natural range of mid- and late-Holocene variability.","PeriodicalId":2,"journal":{"name":"ACS Applied Bio Materials","volume":"8 20","pages":""},"PeriodicalIF":4.7000,"publicationDate":"2024-05-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"ACS Applied Bio Materials","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1139/as-2023-0070","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"MATERIALS SCIENCE, BIOMATERIALS","Score":null,"Total":0}

引用次数: 0

Abstract

Sediment cores were collected from Wrong (WL) and Lenore (LL) lakes in boreal central Yukon Territory, Canada, spanning circa 6000 years. Analyses of pollen, charcoal, magnetic susceptibility, levoglucosan, and down-scaled paleoclimatic data reveal the vegetation history and character/drivers of Holocene fire disturbance. Boreal forest has persisted in the region for millennia, with a regional mid-Holocene expansion of Picea mariana followed by expansion of Pinus contorta in the latest Holocene. The shortest reconstructed fire return intervals (FRI; ca. 110-125 years) occurred in the mid-Holocene, coincident with the development of highly flammable Picea-dominated forest and warm, dry summers that were characterized by elevated JJA Z500 anomalies and associated with an eastward/intense Aleutian Low. In the late-Holocene, FRI increased to ca. 240 years at WL and 280 years LL. Drivers of this change include regional cooling and increased precipitation, with a westward/weaker Aleutian Low position delivering more moisture to interior Yukon. Longer FRIs allowed for greater fuel accumulation between fires, enhancing fire size/severity. While higher fire frequency is noted in the mid-Holocene and increased fire size/severity in the late-Holocene, recent changes in Yukon fire disturbance suggest that the fire regime may soon lie outside the natural range of mid- and late-Holocene variability.

查看原文

微信好友朋友圈 QQ好友复制链接

本刊更多论文

加拿大育空中部北方全新世植被和野火干扰

沉积物岩芯采集自加拿大育空地区中部北方的 Wrong 湖（WL）和 Lenore 湖（LL），时间跨度约 6000 年。对花粉、木炭、磁感应强度、左旋葡聚糖和缩小比例的古气候数据的分析揭示了全新世火灾扰动的植被历史和特征/驱动因素。该地区的北方森林已经存在了数千年，在全新世中期，该地区的马里亚纳松（Picea mariana）面积扩大，随后在全新世晚期，孔雀松（Pinus contorta）面积扩大。重建的最短火灾重返间隔期（FRI；约 110-125 年）出现在全新世中期，与高易燃性 Picea 主导森林的发展以及温暖干燥的夏季相吻合，这些夏季的特点是 JJA Z500 异常值升高，并与向东/强烈的阿留申低气压相关联。在全新世晚期，FRI 在 WL 增加到约 240 年，在 LL 增加到 280 年。这一变化的驱动因素包括区域降温和降水增加，阿留申低地的西移/减弱为育空内陆提供了更多水汽。较长的 FRI 允许在两次火灾之间积累更多的燃料，从而增加了火灾的规模/严重程度。虽然全新世中期火灾频率较高，全新世晚期火灾规模/严重程度增加，但育空火灾干扰的近期变化表明，火灾机制可能很快就会超出全新世中期和晚期的自然变化范围。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

求助全文

约1分钟内获得全文去求助

来源期刊

ACS Applied Bio Materials Chemistry-Chemistry (all)

CiteScore

9.40

自引率

2.10%

发文量

464

期刊介绍： ACS Applied Bio Materials is an interdisciplinary journal publishing original research covering all aspects of biomaterials and biointerfaces including and beyond the traditional biosensing, biomedical and therapeutic applications. The journal is devoted to reports of new and original experimental and theoretical research of an applied nature that integrates knowledge in the areas of materials, engineering, physics, bioscience, and chemistry into important bio applications. The journal is specifically interested in work that addresses the relationship between structure and function and assesses the stability and degradation of materials under relevant environmental and biological conditions.