Abstract

There are not many sites in densely populated temperate Europe where primary forest succession has a chance to run without direct human intervention for a long time and over a relatively large area. The extensive drift sand area of the Veluwe, central Netherlands, provided an opportunity to study succession in a formerly open and dynamic inland sand dune system combining chronosequence and permanent plot approaches. Different successional stages, aged up to 205 years since the first tree individuals established, were identified and vegetation studied using 1200 permanent plots established in 1988 in three adjacent sand dune complexes of different successional age, and resampled during the past three decades. After two centuries, forest succession has proceeded to a pine forest with gradually increasing participation of native deciduous trees. However, their expansion has been arrested by browsing of wild ungulates. Species diversity peaked after about 40 years of forest succession, then declined, and increased again after 100 years. During the past three decades, the herb layer has differentiated in the oldest plots, and the spontaneous forest succession is still in progress. Besides open drift sand with early successional stages, also the spontaneously established late successional forests are valuable from the conservation point of view.

Highlights

  • Dunes cover about 7% of the terrestrial surface of the Earth but only a small portion is still active

  • The succession seems to be divergent at the beginning, when high dunes and plains differ in colonisation by the first species (Ammophila arenaria and Festuca arenaria vs. Polytrichum piliferum, Festuca ovina and Agrostis vinealis)–see the passively projected variables of the relief types

  • The primary forest succession described here represents one of the oldest forest chronosequences in Europe proceeding from bare ground without any direct human interference evident

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Summary

Introduction

Dunes cover about 7% of the terrestrial surface of the Earth but only a small portion is still active. Natural stabilization of dunes can be caused both by abiotic (geomorphologic barriers, changes in wind directions) and biotic factors (ongoing succession). Both types of factors usually operate in concert [1]. Humans have intentionally stabilized many dunes, either by creating artificial barriers or by planting or seeding mostly trees and shrubs to speed up natural stabilization [2]. Succession usually accelerates, but some dunes may remain unstable for thousands of years.

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