当代湿地生态系统恢复问题的古生物学方法

J. Meeder, P. Stone
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摘要

建立一个遗址的历史条件通常是生态系统恢复的第一步。无论是否有可能恢复到历史条件,认识到变化和变化的原因是至关重要的信息。用古生物学方法解决了三种不同的湿地恢复问题。年代地层学在这三个案例中都起到了重要作用,年代际的210Pb和世纪至千年尺度的放射性碳问题。为了记录盐度,我们利用东南盐碱地软体动物群落的变化作为盐度的代表。岩心的垂直变化表明,从1900年开始,盐度随人类世海侵而增加。鉴定了所有岩心的淡水-海水接触,并确定了接触的年代。利用两个相邻岩心之间的时间差异和它们之间的距离来确定海水侵蚀速率,记录了并非所有沿海盆地都表现出相同的速率,并且随着时间的推移,随着海平面上升速度的加快,速率从1960年前的~ 20 m / 1增加到1995年至2017年的> 80 m / 1。这种制度的转变表明,目前的恢复活动是不够的。奥杜邦收购了螺旋沼泽以保护现存最大的木鹳栖息地后不久,沼泽就被筑堤以容纳地表水,因为人们认为周围的土地开发对沼泽水期产生了不利影响。然而,到1970年,柏树再生严重减少,水文和沉积物核心研究开始试图了解变化的驱动因素。基于花粉分析、前期泥炭分析和组织识别,岩心分析表明,在斑片状开放水域泥炭中,水期向上延长。开放水域泥炭表明没有下沉,消除了柏树的发芽。拆除堤坝后不久,柏树开始再生。
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Paleo-Biological Approaches to Present Day Wetland Ecosystem Restoration Problems
Establishing historic conditions of a site is frequently the first step in ecosystem restoration. Whether restoration to historic conditions is possible or not, recognition of change and the cause of change is critical information. Three different wetland restoration problems are addressed by paleo-biological methods. Chrono-stratigraphy was instrumental in all three cases, 210Pb at the decadal and radiocarbon for the century to millennial scale questions. In order to document salinity, change in the Southeast Saline Everglades molluscan assemblages were utilized as a proxy for salinity. Vertical changes in cores established that beginning in ~ 1900 salinity increased with the Anthropocene Marine Transgression. The freshwater-marine contact in all cores was identified and the contacts dated. The differences in time between two adjacent cores and the distance between them was utilized to determine the rate of saltwater encroachment, documenting that not all coastal basins exhibited the same rate and that the rate increased over time in response to the accelerating rate of sea-level rise, increasing from the pre-1960 rate of ~ 20 m yr-1 to > 80 m yr-1 between 1995 and 2017. This shift in regime suggests that present restoration activities are inadequate. Soon after Audubon acquired Corkscrew Swamp to preserve the largest remaining wood stork rookery, the swamp was diked to hold surface water because it was believed that surrounding land development was adversely impacting swamp hydroperiod. However, by 1970 cypress regeneration was severely reduced and hydrology and sediment core studies were initiated in an attempt to understand the driver of the change. Core analysis revealed that hydroperiod increased upwards terminating in patchy open-water peats, based upon pollen analysis, previous peat analysis and tissue recognition. Open-water peats indicate no drawdown, eliminating cypress germination. Cypress regeneration began soon after removal of the dike.
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