植物生态学报 ›› 2010, Vol. 34 ›› Issue (10): 1165-1173.DOI: 10.3773/j.issn.1005-264x.2010.10.005
孙菊1,2, 李秀珍1,*(), 王宪伟1,2, 吕久俊1,2, 李宗梅1,2, 胡远满1
收稿日期:
2009-12-28
接受日期:
2010-02-01
出版日期:
2010-12-28
发布日期:
2010-10-31
通讯作者:
李秀珍
作者简介:
* E-mail: landscape2001@sina.com
SUN Ju1,2, LI Xiu-Zhen1,*(), WANG Xian-Wei1,2, LÜ Jiu-Jun1,2, LI Zong-Mei1,2, HU Yuan-Man1
Received:
2009-12-28
Accepted:
2010-02-01
Online:
2010-12-28
Published:
2010-10-31
Contact:
LI Xiu-Zhen
摘要:
采用除趋势典范对应分析法(DCCA), 对大兴安岭24个冻土湿地植物群落进行排序, 对划分出的3个不同类型多年冻土区的湿地植物群落的物种多样性, 以及生活型和水分生态型等生态特征进行了环境梯度分析。结果表明: 随着纬度的降低, 年平均气温和年平均日照时间逐渐增大, 年平均降水量和年平均湿度逐渐减小, 调查的24个冻土湿地可划分为3组。从大片多年冻土区到大片-岛状多年冻土区, 再到稀疏岛状多年冻土区, 灌木多样性逐渐减小(p < 0.05), 草本植物多样性逐渐增加(p < 0.05); 中生植物种类所占比例分别为38.5%、55.9%和64.4%, 沼生植物的重要值逐渐减小(p < 0.05), 中生和旱生植物的重要值逐渐增大(p < 0.05), 表明冻土湿地的土壤水分条件逐渐中生化, 甚至出现旱生化趋势。地面芽植物在3个多年冻土区的湿地植物群落中始终占优势地位, 高位芽和地下芽植物次之, 反映了该区冬季漫长、严寒而潮湿, 夏季较短的气候特征。大片-岛状多年冻土区作为大片多年冻土区和稀疏岛状多年冻土区的过渡区, 其湿地植物群落的物种多样性和生态特征与稀疏岛状多年冻土区更相近。
孙菊, 李秀珍, 王宪伟, 吕久俊, 李宗梅, 胡远满. 大兴安岭冻土湿地植物群落结构的环境梯度分析. 植物生态学报, 2010, 34(10): 1165-1173. DOI: 10.3773/j.issn.1005-264x.2010.10.005
SUN Ju, LI Xiu-Zhen, WANG Xian-Wei, LÜ Jiu-Jun, LI Zong-Mei, HU Yuan-Man. Analysis of structures of permafrost wetland plant communities along environmental gradients in the Da Hinggan Mountains, China. Chinese Journal of Plant Ecology, 2010, 34(10): 1165-1173. DOI: 10.3773/j.issn.1005-264x.2010.10.005
图2 24个多年冻土湿地植物群落的DCCA二维排序图。 Al, 海拔; H, 年平均湿度; La, 纬度; Lo, 经度; P, 年平均降水量; S, 年平均日照时间; T, 年平均气温。I, 大片多年冻土区; II, 大片-岛状多年冻土区; III, 稀疏岛状多年冻土区; 1-24, 样地。
Fig. 2 Two-dimensional DCCA ordination diagram of 24 permafrost wetlands plant communities. Al, altitude; La, latitude; H, mean annual humidity; Lo, longitude; P, mean annual precipitation; S, mean annual sunshine; T, mean annual air temperature. I, predominantly continuous permafrost; II, predominantly continuous and island permafrost; III, sparely island permafrost; 1-24, sampling sites.
冻土区类型 Permafrost type | 大片多年冻土区 Predominantly continuous permafrost | 大片-岛状多年冻土区 Predominantly continuous and island permafrost | 稀疏岛状多年冻土区 Sparely island permafrost |
---|---|---|---|
样地 Sampling sites | 1-16 | 17-20 | 21-24 |
纬度 Latitude (N) | 50.69°-53.20° | 49.57°-50.38° | 48.83°-49.20° |
经度 Longitude (E) | 121.52°-123.00° | 121.23°-121.71° | 120.80°-121.31° |
海拔 Altitude (m) | 443-836 | 748-817 | 680-782 |
年平均气温 Mean annual air temperature (℃) | -4.2a | -3.0b | -1.1c |
年平均降水量 Mean annual precipitation (mm) | 437.2a | 431.1ab | 423.4b |
年平均湿度 Mean annual humidity (%) | 69.8a | 68.3b | 65.7c |
年平均日照时间 Mean annual sunshine time (h) | 2 450.8a | 2 586.7b | 2 680.7c |
多年冻土的连续性 Continuity of permafrost | 75%-60% | 60%-30% | < 30% |
群落描述 Description of communities | 主要优势灌木和草本植物为柴桦(Betula fruticosa)和白毛羊胡子草(Eriophorum vaginatum), 泥炭藓(Sphagnum spp.)的盖度为0-90% The main dominant shrubs and herbaceous plants were Betula fruticosa and Eriophorum vaginatum. The coverage of Sphagnum spp. was 0-90%. | 主要优势灌木和草本植物为柴桦(B. fruticosa)和大穗薹草 (Carex rhynchophysa), 无泥炭藓(Sphagnum spp.) The main dominant shrubs and herbaceous plants were B. fruticosa and Carex rhynchophysa. There was no Sphagnum spp. in 24 plots. | 主要优势灌木和草本植物为卷边柳(Salix siuzerii)和臌囊薹草(C. schmidtii), 无泥炭藓(Sphagnum spp.) The main dominant shrubs and herbaceous plants were Salix siuzerii and C. schmidtii. There was no Sphagnum spp. in 24 plots. |
表1 3个类型多年冻土区的环境特征
Table 1 Environmental characteristics in the three types of permafrost
冻土区类型 Permafrost type | 大片多年冻土区 Predominantly continuous permafrost | 大片-岛状多年冻土区 Predominantly continuous and island permafrost | 稀疏岛状多年冻土区 Sparely island permafrost |
---|---|---|---|
样地 Sampling sites | 1-16 | 17-20 | 21-24 |
纬度 Latitude (N) | 50.69°-53.20° | 49.57°-50.38° | 48.83°-49.20° |
经度 Longitude (E) | 121.52°-123.00° | 121.23°-121.71° | 120.80°-121.31° |
海拔 Altitude (m) | 443-836 | 748-817 | 680-782 |
年平均气温 Mean annual air temperature (℃) | -4.2a | -3.0b | -1.1c |
年平均降水量 Mean annual precipitation (mm) | 437.2a | 431.1ab | 423.4b |
年平均湿度 Mean annual humidity (%) | 69.8a | 68.3b | 65.7c |
年平均日照时间 Mean annual sunshine time (h) | 2 450.8a | 2 586.7b | 2 680.7c |
多年冻土的连续性 Continuity of permafrost | 75%-60% | 60%-30% | < 30% |
群落描述 Description of communities | 主要优势灌木和草本植物为柴桦(Betula fruticosa)和白毛羊胡子草(Eriophorum vaginatum), 泥炭藓(Sphagnum spp.)的盖度为0-90% The main dominant shrubs and herbaceous plants were Betula fruticosa and Eriophorum vaginatum. The coverage of Sphagnum spp. was 0-90%. | 主要优势灌木和草本植物为柴桦(B. fruticosa)和大穗薹草 (Carex rhynchophysa), 无泥炭藓(Sphagnum spp.) The main dominant shrubs and herbaceous plants were B. fruticosa and Carex rhynchophysa. There was no Sphagnum spp. in 24 plots. | 主要优势灌木和草本植物为卷边柳(Salix siuzerii)和臌囊薹草(C. schmidtii), 无泥炭藓(Sphagnum spp.) The main dominant shrubs and herbaceous plants were Salix siuzerii and C. schmidtii. There was no Sphagnum spp. in 24 plots. |
图3 不同类型多年冻土区湿地植物的多样性变化。 不同小写字母表示差异显著(p < 0.01)。I、II、III, 同图2。
Fig. 3 Changes of species diversity of marsh plants in different types of permafrost. Different small letters indicate significant difference at 0.05 level. I, II, III, see Fig. 2.
生活型 Life form | 大片多年冻土区 Predominantly continuous permafrost | 大片-岛状多年冻土区 Predominantly continuous and island permafrost | 稀疏岛状多年冻土区 Sparely island permafrost | df | F 值 F value |
---|---|---|---|---|---|
高位芽植物 Phanerophytes | 1.047a | 1.000b | 1.000b | 2 | 7.816* |
地上芽植物 Chamaephytes | 0.004a | 0.001a | 0.000a | 2 | 0.292 |
地面芽植物 Hemicryptophytes | 0.866a | 0.819a | 0.825a | 2 | 0.920 |
地下芽植物 Geophytes | 0.079a | 0.177b | 0.168b | 2 | 6.127* |
一年生植物 Therophytes | 0.003a | 0.002a | 0.007a | 2 | 0.381 |
表2 3个类型多年冻土区湿地植物各生活型的重要值
Table 2 Importance values of life forms of wetland plants in the three types of permafrost
生活型 Life form | 大片多年冻土区 Predominantly continuous permafrost | 大片-岛状多年冻土区 Predominantly continuous and island permafrost | 稀疏岛状多年冻土区 Sparely island permafrost | df | F 值 F value |
---|---|---|---|---|---|
高位芽植物 Phanerophytes | 1.047a | 1.000b | 1.000b | 2 | 7.816* |
地上芽植物 Chamaephytes | 0.004a | 0.001a | 0.000a | 2 | 0.292 |
地面芽植物 Hemicryptophytes | 0.866a | 0.819a | 0.825a | 2 | 0.920 |
地下芽植物 Geophytes | 0.079a | 0.177b | 0.168b | 2 | 6.127* |
一年生植物 Therophytes | 0.003a | 0.002a | 0.007a | 2 | 0.381 |
水分生态型 Hydro-ecotype | 大片多年冻土区 Predominantly continuous permafrost | 大片-岛状多年冻土区 Predominantly continuous and island permafrost | 稀疏岛状多年冻土区 Sparely island permafrost | df | F 值 F value |
---|---|---|---|---|---|
沼生植物 Helophytes | 0.809a | 0.593a | 0.147b | 2 | 13.956* |
湿生植物 Hygrophytes | 0.845a | 0.751a | 1.072b | 2 | 6.571* |
中生植物 Mesophytes | 0.346a | 0.651b | 0.775b | 2 | 7.681* |
旱生植物 Xerophils | 0.001a | 0.005b | 0.006ab | 2 | 4.060* |
表3 3个类型多年冻土区湿地植被各水分生态型的重要值
Table 3 Importance values of hydro-ecotypes of wetland vegetation in the three types of permafrost
水分生态型 Hydro-ecotype | 大片多年冻土区 Predominantly continuous permafrost | 大片-岛状多年冻土区 Predominantly continuous and island permafrost | 稀疏岛状多年冻土区 Sparely island permafrost | df | F 值 F value |
---|---|---|---|---|---|
沼生植物 Helophytes | 0.809a | 0.593a | 0.147b | 2 | 13.956* |
湿生植物 Hygrophytes | 0.845a | 0.751a | 1.072b | 2 | 6.571* |
中生植物 Mesophytes | 0.346a | 0.651b | 0.775b | 2 | 7.681* |
旱生植物 Xerophils | 0.001a | 0.005b | 0.006ab | 2 | 4.060* |
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