Schuster W S F, Griffin K L, Roth H, Turnbull M H, Whitehead D, Tissue D T
Black Rock Forest Consortium, Cornwall, NY 12518, USA.
Tree Physiol. 2008 Apr;28(4):537-49. doi: 10.1093/treephys/28.4.537.
We sought to quantify changes in tree species composition, forest structure and aboveground forest biomass (AGB) over 76 years (1930-2006) in the deciduous Black Rock Forest in southeastern New York, USA. We used data from periodic forest inventories, published floras and a set of eight long-term plots, along with species-specific allometric equations to estimate AGB and carbon content. Between the early 1930s and 2000, three species were extirpated from the forest (American elm (Ulmus americana L.), paper birch (Betula papyrifera Marsh.) and black spruce (Picea mariana (nigra) (Mill.) BSP)) and seven species invaded the forest (non-natives tree-of-heaven (Ailanthus altissima (Mill.) Swingle) and white poplar (Populus alba L.) and native, generally southerly distributed, southern catalpa (Catalpa bignonioides Walt.), cockspur hawthorn (Crataegus crus-galli L.), red mulberry (Morus rubra L.), eastern cottonwood (Populus deltoides Bartr.) and slippery elm (Ulmus rubra Muhl.)). Forest canopy was dominated by red oak and chestnut oak, but the understory tree community changed substantially from mixed oak-maple to red maple-black birch. Density decreased from an average of 1500 to 735 trees ha(-1), whereas basal area doubled from less than 15 m(2) ha(-1) to almost 30 m(2) ha(-1) by 2000. Forest-wide mean AGB from inventory data increased from about 71 Mg ha(-1) in 1930 to about 145 Mg ha(-1) in 1985, and mean AGB on the long-term plots increased from 75 Mg ha(-1) in 1936 to 218 Mg ha(-1) in 1998. Over 76 years, red oak (Quercus rubra L.) canopy trees stored carbon at about twice the rate of similar-sized canopy trees of other species. However, there has been a significant loss of live tree biomass as a result of canopy tree mortality since 1999. Important constraints on long-term biomass increment have included insect outbreaks and droughts.
我们试图量化美国纽约东南部落叶阔叶林黑岩森林在76年(1930 - 2006年)间树种组成、森林结构和地上森林生物量(AGB)的变化。我们使用了定期森林清查数据、已发表的植物志以及一组8个长期样地的数据,结合特定物种的异速生长方程来估算AGB和碳含量。在20世纪30年代早期至2000年间,森林中有3个物种灭绝(美国榆(Ulmus americana L.)、纸桦(Betula papyrifera Marsh.)和黑云杉(Picea mariana (nigra) (Mill.) BSP)),7个物种侵入森林(外来物种臭椿(Ailanthus altissima (Mill.) Swingle)和银白杨(Populus alba L.)以及本地物种、通常分布在南方的南方梓树(Catalpa bignonioides Walt.)、鸡距山楂(Crataegus crus-galli L.)、红桑(Morus rubra L.)、东部杨(Populus deltoides Bartr.)和滑榆(Ulmus rubra Muhl.))。森林冠层以红栎和栗栎为主,但林下树木群落从混合的栎树 - 枫树群落大幅转变为红枫 - 黑桦群落。密度从平均每公顷1500棵树降至735棵,而到2000年,断面积从每公顷不到15平方米翻倍至近30平方米。清查数据显示,全森林范围的平均AGB从1930年的约71 Mg/公顷增加到1985年的约145 Mg/公顷,长期样地的平均AGB从1936年的75 Mg/公顷增加到1998年的218 Mg/公顷。在76年里,红栎(Quercus rubra L.)冠层树木储存碳的速率约为其他类似大小冠层树木的两倍。然而,自1999年以来,由于冠层树木死亡,活树生物量出现了显著损失。长期生物量增加的重要限制因素包括虫害爆发和干旱。