Brncic Terry M, Willis Katherine J, Harris David J, Washington Richard
Oxford Long-term Ecology Laboratory, Oxford University Centre for the Environment, South Parks Road, Oxford OX1 3QY, UK.
Philos Trans R Soc Lond B Biol Sci. 2007 Feb 28;362(1478):229-42. doi: 10.1098/rstb.2006.1982.
This paper presents the results from a palaeoecological study to establish the impact of prehistoric human activity and climate change on the vegetation and soils of the Goualougo area of the Nouabalé-Ndoki National Park, in the Republic of Congo (Congo-Brazzaville). This is a region that is known from previous work (through evidence of pottery, furnaces and charcoal layers beneath the present day rainforest vegetation) to have had prehistoric settlement dating back to at least 2000 calibrated years before present. In addition, there is climatic evidence to suggest that significant variations in precipitation have occurred in central Africa over the last few millennia. Presently, the region is covered in uninhabited moist semi-evergreen rainforest. Key research questions addressed in this paper include the extent to which the present-day composition of rainforest in this region is as a result of processes of the past (climate change and/or human activity), and the resilience of the rainforest to these perturbations. Statistical analyses of pollen, microscopic charcoal and geochemical data are used to determine the relationship over time between vegetation dynamics and climate change, anthropogenic burning and metal smelting. Significant changes in forest composition are linked to burning and climate change but not metallurgy. The strongest influence on the present day composition appears to be related to the increased anthropogenic burning that started approximately 1000 years ago. Results from this study are discussed in terms of their implications for the present and future management of this globally important forested region.
本文展示了一项古生态研究的结果,该研究旨在确定史前人类活动和气候变化对刚果共和国(刚果布拉柴维尔)诺阿巴莱-恩多基国家公园瓜洛古地区植被和土壤的影响。根据此前的研究工作(通过现今雨林植被下陶器、熔炉和木炭层的证据)可知,该地区曾有过史前定居点,可追溯到距今至少2000年的校正年代。此外,有气候证据表明,在过去几千年里,非洲中部的降水量发生了显著变化。目前,该地区覆盖着无人居住的湿润半常绿雨林。本文探讨的关键研究问题包括,该地区现今雨林的组成在多大程度上是过去各种过程(气候变化和/或人类活动)的结果,以及雨林对这些扰动的恢复力。通过对花粉、微观木炭和地球化学数据的统计分析,来确定植被动态与气候变化、人为燃烧和金属冶炼之间随时间的关系。森林组成的显著变化与燃烧和气候变化有关,但与冶金无关。对现今组成影响最大的似乎与大约1000年前开始的人为燃烧增加有关。本文从这些结果对这个全球重要森林地区当前和未来管理的影响方面进行了讨论。