Lovelock Catherine E, Feller Ilka C, Ellis Joanne, Schwarz Ann Maree, Hancock Nicole, Nichols Pip, Sorrell Brian
Centre for Marine Studies, University of Queensland, St Lucia, Queensland, Australia.
Oecologia. 2007 Sep;153(3):633-41. doi: 10.1007/s00442-007-0750-y. Epub 2007 May 10.
Mangrove forest coverage is increasing in the estuaries of the North Island of New Zealand, causing changes in estuarine ecosystem structure and function. Sedimentation and associated nutrient enrichment have been proposed to be factors leading to increases in mangrove cover, but the relative importance of each of these factors is unknown. We conducted a fertilization study in estuaries with different sedimentation histories in order to determine the role of nutrient enrichment in stimulating mangrove growth and forest development. We expected that if mangroves were nutrient-limited, nutrient enrichment would lead to increases in mangrove growth and forest structure and that nutrient enrichment of trees in our site with low sedimentation would give rise to trees and sediments that converged in terms of functional characteristics on control sites in our high sedimentation site. The effects of fertilizing with nitrogen (N) varied among sites and across the intertidal zone, with enhancements in growth, photosynthetic carbon gain, N resorption prior to leaf senescence and the leaf area index of canopies being significantly greater at the high sedimentation sites than at the low sedimentation sites, and in landward dwarf trees compared to seaward fringing trees. Sediment respiration (CO(2) efflux) was higher at the high sedimentation site than at the low one sedimentation site, but it was not significantly affected by fertilization, suggesting that the high sedimentation site supported greater bacterial mineralization of sediment carbon. Nutrient enrichment of the coastal zone has a role in facilitating the expansion of mangroves in estuaries of the North Island of New Zealand, but this effect is secondary to that of sedimentation, which increases habitat area and stimulates growth. In estuaries with high sediment loads, enrichment with N will cause greater mangrove growth and further changes in ecosystem function.
新西兰北岛河口的红树林覆盖面积正在增加,这导致河口生态系统的结构和功能发生变化。沉积物淤积及相关的养分富集被认为是导致红树林覆盖面积增加的因素,但这些因素各自的相对重要性尚不清楚。我们在具有不同沉积历史的河口进行了一项施肥研究,以确定养分富集在刺激红树林生长和森林发育中的作用。我们预计,如果红树林受到养分限制,养分富集将导致红树林生长和森林结构增加,并且在我们低沉积区域施肥的树木所产生的树木和沉积物在功能特征上会与我们高沉积区域的对照地点趋同。施氮(N)的效果在不同地点和潮间带有所不同,高沉积地点的生长、光合碳吸收、叶片衰老前的氮素再吸收以及树冠的叶面积指数的增加显著高于低沉积地点,并且与向海边缘树木相比,内陆矮树的增加更为明显。高沉积地点的沉积物呼吸(CO₂ 通量)高于低沉积地点,但施肥对其没有显著影响,这表明高沉积地点支持更大程度的沉积物碳细菌矿化。沿海地区的养分富集在促进新西兰北岛河口红树林扩张方面具有一定作用,但这种影响仅次于沉积物淤积,沉积物淤积增加了栖息地面积并刺激了生长。在沉积物负荷高的河口,氮富集将导致更大的红树林生长和生态系统功能的进一步变化。