Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China; Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China; Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China.
Sci Total Environ. 2023 Dec 15;904:166962. doi: 10.1016/j.scitotenv.2023.166962. Epub 2023 Sep 9.
In southern China, Chinese fir Cunninghamia lanceolata is one of the most important native conifer trees, widely used in afforestation programs. This area has the largest forestland atmospheric carbon sink, and a relatively young stand age characterizes these forests. However, how C. lanceolata forests evolved regarding their ability to sequester carbon remains unclear. Here we present data on carbon storage and sequestration capacity of C. lanceolata at six stand ages (5-, 10-, 15-, 20-, 30- and 60 - year-old stands). Results show that the carbon stock in trees, understory, vegetation, litter, soil, and ecosystem significantly increased with forest age. The total ecosystem carbon stock increased from 129.11 to 348.43 Mg ha in the 5- and 60 - year-old stands. The carbon sequestration rate of C. lanceolata shows an overall increase in the first two stand intervals (5-10 and 10-15), peaks in the 15-20 stand intervals, and then decreases in the 20-30 and 30-60 stand intervals. Our result revealed that carbon sequestration rate is a matter of tree age, with the highest sequestration rates occurring in the middle age forest (15-20 - year-old). Therefore, this information may be useful for national climate change mitigation actions and afforestation programs, since forests are primarily planted for this purpose.
在中国南方,杉木(Cunninghamia lanceolata)是最重要的乡土针叶树种之一,广泛用于造林计划。该地区拥有最大的林地大气碳汇,这些森林的特点是相对年轻的林龄。然而,杉木林在固碳能力方面是如何演变的尚不清楚。本研究提供了 6 个林龄(5 年、10 年、15 年、20 年、30 年和 60 年)杉木林的碳储量和固碳能力数据。结果表明,树木、林下植被、植被、凋落物、土壤和生态系统中的碳储量随林龄显著增加。在 5 年生和 60 年生林分中,总生态系统碳储量从 129.11 增加到 348.43 Mg·ha-1。杉木的碳固存率在前两个林龄间隔(5-10 年和 10-15 年)呈总体增加趋势,在 15-20 年林龄间隔达到峰值,然后在 20-30 年和 30-60 年林龄间隔下降。本研究结果表明,碳固存率是树龄的一个问题,中龄林(15-20 年生)的固存率最高。因此,这些信息可能对国家气候变化缓解行动和造林计划有用,因为森林主要是为此目的而种植的。