Response of African humid tropical forests to recent rainfall anomalies

During the last decade, strong negative rainfall anomalies resulting from increased sea surface temperature in the tropical Atlantic have caused extensive droughts in rainforests of western Amazonia, exerting persistent effects on the forest canopy. In contrast, there have been no significant impacts on rainforests of West and Central Africa during the same period, despite large-scale droughts and rainfall anomalies during the same period. Using a combination of rainfall observations from meteorological stations from the Climate Research Unit (CRU; 1950–2009) and satellite observations of the Tropical Rainfall Measuring Mission (TRMM; 1998–2010), we show that West and Central Africa experienced strong negative water deficit (WD) anomalies over the last decade, particularly in 2005, 2006 and 2007. These anomalies were a continuation of an increasing drying trend in the region that started in the 1970s. We monitored the response of forests to extreme rainfall anomalies of the past decade by analysing the microwave scatterometer data from QuickSCAT (1999–2009) sensitive to variations in canopy water content and structure. Unlike in Amazonia, we found no significant impacts of extreme WD events on forests of Central Africa, suggesting potential adaptability of these forests to short-term severe droughts. Only forests near the savanna boundary in West Africa and in fragmented landscapes of the northern Congo Basin responded to extreme droughts with widespread canopy disturbance that lasted only during the period of WD. Time-series analyses of CRU and TRMM data show most regions in Central and West Africa experience seasonal or decadal extreme WDs (less than −600 mm). We hypothesize that the long-term historical extreme WDs with gradual drying trends in the 1970s have increased the adaptability of humid tropical forests in Africa to droughts.     

树木年轮揭示的东灵山主要树种间干旱耐受性差异

近年来北京地区的森林随极端干旱加剧表现出脆弱性特征,为了解气候变化下不同树种的干旱耐受性,选择北京东灵山森林内3个乔木树种(华北落叶松、油松和辽东栎),利用树木年轮生态学方法分析了径向生长与气候的关系,以及对极端干旱事件的抵抗力和弹性。结果表明: 华北落叶松和油松与5—6月气温呈显著负相关,辽东栎与5月气温呈显著负相关;华北落叶松与6月降水量、5—6月和8—9月相对湿度呈显著正相关,油松与6—8月降水量和相对湿度呈显著正相关,辽东栎与2月和5月降水量、5月相对湿度呈显著正相关;所有树种均与当年5—7月标准化降水蒸散指数(SPEI)呈显著正相关。华北落叶松是干旱耐受性最弱的树种,径向生长在所选极端干旱事件中(1994年、2001—2002年和2007年)下降幅度最大(46.6%～69.6%),抵抗力(0.534、0.304、0.530)和弹性(0.686、0.570、0.753)显著低于辽东栎和油松,辽东栎在2007年抵抗力显著高于油松,弹性无显著差异。生长季持续的高温或降水减少引起的极端干旱是树木径向生长下降的主要原因,树种间各异的生理生态策略是干旱耐受性差异的可能原因。研究结果可为未来造林树种选择和森林管护措施制定提供新依据,以在气候压力持续增加背景下维持森林生态系统功能和服务。     

Persistence of seed banks in Australian temporary wetlands

1. The ability of seeds to survive periods of drying and wetting that do not lead to seed production will determine the potential species pool for future plant communities of temporary wetlands. I investigated characteristics of the seed banks in sediment from Australian temporary wetlands that might contribute to the ability of aquatic plants to re‐establish after extended drought. 2. Experimental investigation into germination from sediment from six sites in five Australian temporary wetlands, with various water regimes, examined two sources of seed bank depletion: (i) length of time dry (longevity up to 12 years) and (ii) successive annual wetting and germination events (up to seven) with intervening periods dry (leaving a residual seed bank), both without any opportunity for replenishment of the seed bank. 3. These wetlands had species‐rich, long‐lived seed banks that were not exhausted by successive germination events. After three years of dry storage, 90% of the original seed bank species germinated, after six years 75% and after 12 years 20%. After seven successive wetting and drying events without seed bank replenishment, 48% of the original species still germinated. The mean survival time dry for seed bank species, 7.4 years, was longer than the duration of recent droughts. 4. Seed bank composition varied among wetlands and over time; most species did not occur in all wetlands and many occurred in one wetland only. The germination patterns of different species, although differing in detail, tended to be consistent in that all species could survive long dry periods and several wetting and drying events. However, experimental drought significantly diminished species richness and abundance, indicating limits to seed bank persistence. 5. Data from such long‐term studies of seed bank persistence should allow prediction of the species richness and composition of the germinating communities in a wetland whose water regime is intentionally or unintentionally altered. This ability to forecast may become particularly important under climate change and the need to predict future wetland conditions.