Ecosystem Development and Plant Succession on Landslides in the Caribbean

Lawrence R. Walker; Daniel J. Zarin; Ned Fetcher; Randall W. Myster; Arthur H. Johnson

doi:10.2307/2389097

Ecosystem Development and Plant Succession on Landslides in the Caribbean

Biotropica ◽

10.2307/2389097 ◽

1996 ◽

Vol 28 (4) ◽

pp. 566 ◽

Cited By ~ 117

Author(s):

Lawrence R. Walker ◽

Daniel J. Zarin ◽

Ned Fetcher ◽

Randall W. Myster ◽

Arthur H. Johnson

Keyword(s):

Plant Succession ◽

Ecosystem Development ◽

The Caribbean

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Of mosses and men: Plant succession, soil development and soil carbon accretion in the sub-Arctic volcanic landscape of Hekla, Iceland

Progress in Physical Geography Earth and Environment ◽

10.1177/0309133318798754 ◽

2018 ◽

Vol 42 (6) ◽

pp. 765-791 ◽

Cited By ~ 1

Author(s):

Olga Kolbrún Vilmundardóttir ◽

Friðþór Sófus Sigurmundsson ◽

Gro Birkefeldt Møller Pedersen ◽

Joaquín Muñoz-Cobo Belart ◽

Fadi Kizel ◽

...

Keyword(s):

Soil Carbon ◽

Loose Material ◽

Soil Development ◽

Lava Flows ◽

Plant Succession ◽

Mean Annual Precipitation ◽

Soil Parameters ◽

Mean Annual Temperature ◽

Ecosystem Development ◽

Soil Accumulation

Lava flows pose a hazard in volcanic environments and reset ecosystem development. A succession of dated lava flows provides the possibility to estimate the direction and rates of ecosystem development and can be used to predict future development. We examine plant succession, soil development and soil carbon (C) accretion on the historical (post 874 AD) lava flows formed by the Hekla volcano in south Iceland. Vegetation and soil measurements were conducted all around the volcano reflecting the diverse vegetation communities on the lavas, climatic conditions around Hekla mountain and various intensities in deposition of loose material. Multivariate analysis was used to identify groups with similar vegetation composition and patterns in the vegetation. The association of vegetation and soil parameters with lava age, mean annual temperature, mean annual precipitation and soil accumulation rate (SAR) was analysed. Soil carbon concentration increased with increasing lava age becoming comparable to concentrations found on the prehistoric lavas. The combination of a sub-Arctic climate, gradual soil thickening due to input of loose material and the specific properties of volcanic soils allow for continuing accumulation of soil carbon in the soil profile. Four successional stages were identified: initial colonization and cover coalescence (ICC) of Racomitrium lanuginosum and Stereocaulon spp. (lavas <70 years of age); secondary colonization (SC) – R. lanuginosum dominance (170−700 years); vascular plant dominance (VPD) (>600 years); and highland conditions/retrogression (H/R) by tephra deposition (70−860 years). The long time span of the SC stage indicates arrested development by the thick R. lanuginosum moss mat. The progression from SC into VPD was linked to age of the lava flows and soil depth, which was significantly deeper within the VPD stage. Birch was growing on lavas over 600 years old indicating the development towards birch woodland, the climax ecosystem in Iceland.

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