Fjölrit RALA - 15.01.2001, Side 7

Fjölrit RALA - 15.01.2001, Side 7
SUMMARY Vegetation succession in areas colonized by the introduced Nootka lupin (Lupinus nootkatensisj in Iceland The effect of Nootka lupin on vegetation and soil (0-10 cm) was investigated at 15 sites in southem and northem Iceland. Plant biomass was determined at 10 of the sites. The lupin had been at the sites for 10-40 yrs and colonized barren eroded areas, glacial river beds, partly vegetated moss heaths and denser dwarf-shrub heaths. Transects were laid out and a comparison made of lupin of different age within patches and the adjacent areas outside them. A total of 27 patches was investigated and measurements carried out in 93 plots. In the analysis CANOCO-ordination was used to analyse sucessional trends. In southem Iceland, where annual precipitation is 900-3400 mm, the lupin was of high stature (80-120 cm) and formed a closed canopy. In northem Iceland, where annual precipitaion is 500-800 mm, the lupin was lower in height (40-110 cm) and did not form a closed canopy on the driest gravel flats. There it, however, formed dense patches on dwarf shmb heaths and in coastal areas. Lupin biomass was 300-990 g/m2 in the southem area and 80-650 g/m2 in the northem area. At sites where the lupin formed dense, long-lasting patches it had great effect on the vegetation development. The ordination results revealed that successional changes caused by the lupin tended to go into the same direction irrespective of the type of land it colonized. Within the patches the vegetation developed towards a forb-rich grassland, abundant in horsetails (Equisetum) at some of the sites. In the south Poa pratensis was the dominant grass species at most of the sites, but Poa glauca and Festuca richardsonii in the north. A dense mosslayer developed undemeath the lupin at most of the sourthem sites. The effects of the lupin were generally greater in the southem area and the vegetation of old patches was rather uniform. It was more diverse in the northem area, where the lupin had less pronounced effects on vegetation composition at the drier sites. Species richness was greatly reduced at most of the sites where the lupin formed dense patches. At the southem sites 20-60 plant species were found in plots outside the patches but 5-25 species within the oldest parts of lupin patches. At the northem sites 10-55 species were found on the outsite but 3-62 species within the oldest parts of the patches. The greatest reduction occurred where the lupin had colonized dwaf-shmb heathlands in northem Iceland resulting in disappearance of most of the native species. At the drier northem sites species richness was little affected by the lupin or even mcreased. There, most existing species survived within the open lupin patches and at some of the sites birch (Betula pubescens) colonization occurred which was rare at other sites. The lupin was generally densest close to the edges of patches where the plants had just reached maturity. The lupin density tended to decrease towards the oldest center of the patches. The longevity of the lupin varied, however, greatly between sites. At some of the southem and the drier northem sites the lupin had degenerated in the oldest parts of patches, where it had colonized 15-25 years earlier. At other southem and northem sites the lupin maintained a high cover and was still dominant in the oldest parts of patches where it had been growing for 25-35 years. Most of these sites were from areas of high annual precipitation, late snowmelt in spring or high groundwater table. C and N content of soil increased considerably where the lupin colonized barren or partly vegetated areas. The changes were greatest at sites from the southem area where C increased about 0,1% (-1300 kg/ha) and N 0,01% (-120 kg/ha) per year. There was about tenfold difference in the rate of C and N accumulation in the soil between sites. At sites in the northem area where the lupin had colonized dwarf-shmb heathland with a relatively humus rich soil there were indications of net-carbon loss from the soil. The Nootka lupin is a very effective plant for land reclamation in Iceland. Dense plant cover and soil fertility can be gained within a relatively short time span, where the growth of the lupin is not limited by droughts. The Iupín is well suited for reclamation of large, barren areas. The nitrogen fixation of the lupin, rapid growth, size and patch formation, on the other hand, enables it to invade mossheaths and dwarf-shmb heathlands which it will take over and displace. This calls for strict management guidelines on the future use of the plant in the country. 5
Side 1
Side 2
Side 3
Side 4
Side 5
Side 6
Side 7
Side 8
Side 9
Side 10
Side 11
Side 12
Side 13
Side 14
Side 15
Side 16
Side 17
Side 18
Side 19
Side 20
Side 21
Side 22
Side 23
Side 24
Side 25
Side 26
Side 27
Side 28
Side 29
Side 30
Side 31
Side 32
Side 33
Side 34
Side 35
Side 36
Side 37
Side 38
Side 39
Side 40
Side 41
Side 42
Side 43
Side 44
Side 45
Side 46
Side 47
Side 48
Side 49
Side 50
Side 51
Side 52
Side 53
Side 54
Side 55
Side 56
Side 57
Side 58
Side 59
Side 60
Side 61
Side 62
Side 63
Side 64
Side 65
Side 66
Side 67
Side 68
Side 69
Side 70
Side 71
Side 72
Side 73
Side 74
Side 75
Side 76
Side 77
Side 78
Side 79
Side 80
Side 81
Side 82
Side 83
Side 84
Side 85
Side 86
Side 87
Side 88
Side 89
Side 90
Side 91
Side 92
Side 93
Side 94
Side 95
Side 96
Side 97
Side 98
Side 99
Side 100
Side 101
Side 102
Side 103
Side 104
Side 105
Side 106

x

Fjölrit RALA

Direkte link

Hvis du vil linke til denne avis/magasin, skal du bruge disse links:

Link til denne avis/magasin: Fjölrit RALA
https://timarit.is/publication/1497

Link til dette eksemplar:

Link til denne side:

Link til denne artikel:

Venligst ikke link direkte til billeder eller PDfs på Timarit.is, da sådanne webadresser kan ændres uden advarsel. Brug venligst de angivne webadresser for at linke til sitet.