Tremblay Megan, Stager J Curt, St-Jacques Jeannine-Marie, Murphy Skylar, Peros Matthew, Carl Brian S
Department of Geography, Planning and Environment, Concordia University, Montréal, Québec, Canada.
Department of Natural Sciences, Paul Smith's College, Paul Smiths, New York, United States of America.
PLoS One. 2024 Dec 18;19(12):e0314101. doi: 10.1371/journal.pone.0314101. eCollection 2024.
Two radiocarbon-dated pollen and charcoal records from cores collected at Stump Pond and a wetland in suburban Albany County, New York, provide new insights into the environmental history of a unique inland pine barrens that is currently surrounded and threatened by urban development: the Albany Pine Bush (APB). The Stump Pond core shows that the pond formed roughly 13,000 years ago with the recession of glacial Lake Albany. From ca. 13,000 to 11,000 years ago spruce (Picea) and other boreal forest taxa were more common in the region than they are today, but both cores show that pine-oak (Pinus-Quercus) assemblages similar to those of today's APB have been predominant components of the local forests for the last ca. 11,000 years. Abundant charcoal in both cores demonstrates that fire activity was a frequent occurrence in the APB throughout its history, particularly for the last ca. 6400 years. Water tables rose in response to increasingly humid hydroclimates, leading to the establishment of the wetland site ca. 6400 years ago and a greater abundance of ferns and mosses there during the last millennium. More recently, expanding urbanization and its associated impacts demonstrate that human activity has become the primary driver of change in the APB ecosystem.
从纽约奥尔巴尼县郊区的树桩池塘和一处湿地采集的两份经放射性碳年代测定的花粉和木炭记录,为目前被城市发展包围并受到威胁的独特内陆松瘠地——奥尔巴尼松布什(APB)的环境历史提供了新的见解。树桩池塘的岩芯显示,该池塘大约在13000年前随着奥尔巴尼冰川湖的消退而形成。在大约13000年至11000年前,云杉(云杉属)和其他北方森林类群在该地区比现在更为常见,但两份岩芯都表明,与如今APB的植被组合相似的松树 - 橡树(松属 - 栎属)组合在过去约11000年里一直是当地森林的主要组成部分。两份岩芯中丰富的木炭表明,火灾活动在APB的整个历史中频繁发生,尤其是在过去约6400年。地下水位因气候变得越来越湿润而上升,导致约6400年前该湿地形成,并且在过去一千年里那里的蕨类植物和苔藓更加丰富。最近,城市化的扩张及其相关影响表明,人类活动已成为APB生态系统变化的主要驱动因素。