Alpine treelines online

See the report of the workshop on these pages and the original call on the MRI Website

With a dedicated focus session on alpine treelines!
For more general information about the conference please visit the IMC 2022 website.

Presented by Maaike Bader, April 28, 2021, 15:00 — 16:00 CEST
A recording of the lecture is now available at the Mountain Research Initiative (MRI) website.

Edited by Pavel Moiseev, submissions possible until November 2021.
See the MDPI website for more information.

Posted by: Maaike Bader, November 10, 2020

Examples of treeline forms as described in the new Ecography paper. From left to right and top to bottom: gradual treeline, diffuse treeline, abrupt tree-island treeline, abrupt treeline, abrupt diffuse treeline in shrub matrix, krummholz-island treeline. From Bader et al, early view.

We are very happy to announce the publication of our new paper (open access in Ecography, for download here) addressing the pattern dimensions that we think are most indicative of the processes forming spatial patterns in alpine-treeline ecotones, and redefining some terminology for describing treeline spatial pattern or "form". This paper is the culmination of our discussions during several workshops in the past years, starting with the MRI synthesis workshop in Jaca, Spain, in 2017, followed by the two sTreelines workshops at sDiv (iDiv, Leipzig, Germany) in 2018 and 2019 and a workshop organised by Bradley Case in Hanmer Springs, New Zealand, in 2020.

Apart from defining four main pattern dimensions (two in the x-y plane: 1) changes in tree cover, and 2) changes in the level of clumping; two in cross-section: 3) changes in tree height, and 4) changes in tree shape), we here also suggest a more precise terminology for describing treeline forms. In particular, we suggest to use two different terms for describing the smoothness of the transition: if there is a sudden strong frop in tree HEIGHT the treeline is "abrupt", but if only the decrease in tree COVER is sudden and strong, this treeline is "discrete". If both change suddenly and strongly, the treeline is still "abrupt", because we consider discreteness as the default. At the other end, if tree HEIGHT decreases gradually, the treeline is "gradual", but if tree COVER decreases gradually, the treeline is "diffuse". If both decrease gradually, the treeline is still "diffuse", because we consider a gradual height decline as the default. Now one can guess what an abrupt diffuse treeline looks like... Additionally, there are tree-island and krummholz-island treelines and some other forms... I recommend reading the paper for more details and further insights :-)

You may also check out our blogpost on the Ecography website.

An abrupt (and discrete, which is the default so it does not need to be mentioned) treeline formed by Lophozonia menziesii (Nothofagaceae) near Lewis´ Pass on the South Island of New Zealand.

Reference: Bader, M.Y., L.D. Llambí, B.S. Case, H.L. Buckley, J.M. Toivonen, J.J. Camarero, D.M. Cairns, C.D. Brown, T. Wiegand and L.M. Resler (2021) A global framework for linking alpine-treeline ecotone patterns to underlying processes. Ecography 44(2): 265-292, DOI 10.1111/ecog.05285.

By: Maaike Bader, September 19, 2019

Treeline excursion with some of the workshop participants to Mt. Patscherkofel. Photo looking west down into the Inn valley west of Innsbruck. Tree species: spruce (Picea abies) and, most abundant at the highest elevation, Swiss stone pine (Pinus cembra).

At the International Mountain Conference, held in Innsbruck from September 9 to 12, 2019, treeline and mountain forest researchers from many parts of the world (including Japan, Australia, Venezuela, Brasil, Italy, France, Finland, Germany, and of course Austria and Switzerland) met in and around the "The Future of Mountain Forests" workshop and poster session, the program of which can be downloaded here.

The workshop, attended by about 100 people, including presenting participants and public, was divided by the moderators into three topical sections: treelines, stress and disturbance, and management. Apart from short (3-minute) presentations, the workshop consisted of discussions about the importance, main factors and research needs for each topic. Treeline-related presentations addressed drivers of treeline shifts, including those affecting seedling establishment (viable seed availability and interactions with alpine vegetation) and those affecting tree growth (drought, growing-season temperature, frost damage, competition), as well as landscape-scale variation in tree performance (establishment or persistence) at treeline and the role of topography and potential indicative value of treeline ecotone spatial patterns. Of course there was a lot of thematic overlap between the sections, the treeline section including contributions about stress and the management section including various contributions about disturbances (the function of forests killed by bark beetle outbreaks or otherwise affected by climate change and disturbances on forest protective functions) and one about montane forest-grassland ecotones (Brasilian Antlantic forest fragments that are stabilised in a grass matrix) with properties and processes potentially resembling those at alpine treeline ecotones.

The main research needs related to treelines that were identified include: more attention for soil processes, nutrients and mycorrhiza; using demographic processes and age structures to understand treeline dynamics; using spatial patterns and dynamics for understanding processes; identifying species-specific requirements for recruitment; identfying species-specific growth responses to e.g. temperature, moisture and stress and disturbance factors; identifying sensitivities specific to different ontogenetic stages; understanding (historic) land-use effects; improving the global coverage and distribution of research efforts.

On Friday, some of us took advantage of the great weather to visit Mt. Patscherkofel, passing through a treeline ecotone quite strongly determined by former land use and arguably restricted in its advance due to the "summit syndrome" present on this Föhn- affected rounded mountain. What is likely not limiting here is seed dispersal, judging from the high abundance of nutcrackers, which can disperse Pinus cembra well into the alpine zone. Apart form the close-by view, Mt Patscherkofel provided wonderful views of the surrounding mountains and treeline ecotones. We discussed how much of the landscape has been completely deforested a few centuries ago and the implications for our interpretation of the current treeline ecotones in the Alps. Keep an eye out for the next International Mountain Conference (IMC 2022, Innsbruck, 12-15 Sept 2022).

By: Maaike Bader, September 6, 2019

Treeline composed of larch (Larix decidua) and mountain pine (Pinus uncinata) near the Lautaret Pass, French Alps. Picture taken from a South-facing looking at a North-facing slope.

The idea for this website was born during a synthesis workshop about treeline spatial patterns , held in Jaca (Spain) in 2017. We wanted to provide a platform to share data and exchange ideas about the patterns that can be observed in treeline ecotones (= ecological transition zones) worldwide and the processes that form these patterns and that also determine treeline dynamics. Apart from our scientific interest in understanding the ecology of treeline ecotones, another motivation for this is that alpine (and arctic) treelines, being strongly controlled by climate, are likely to be directly affected by climate change. Expected is an upward (or poleward) shift in treeline position as more warmth becomes available for tree growth. However, the rate of such shifts depends not only on the temperature-controlled growth rate of the trees, but also on many other ecological processes such as seed production and dispersal, seedling establishment, interactions with neighbouring trees and other vegetation, seed predation and herbivory, climate-induced damage and geomorphic disturbances. Depending on the relative importance of these processes, treelines are expected to differ in their spatial patterns as well as dynamics in response to climatic change. This website aims to bring together information about the occurrence of different spatial patterns at treelines wordlwide, about known relationships between patterns and processes, and about methods to study such relationships.

A database facility for scientific data about treeline ecotones is planned for a later stage. At this stage, you will find a map of treeline sites (see Explore treelines) providing basic ecological information and images of these sites, and an invitation to contribute more sites to this map. This invitation is open to anybody that has visited or is planning to visit mountain areas with treelines and that is willing and able to follow the instructions provided (see Instructions for data contributors). The simplest form of instructions is: take a picture that shows the treeline, look up the coordinates of the site on Google Earth or Bing Maps, and send us the picture, site name and coordinates per email. While developing a more sophisticated data management system, we currenlty provide interested site contributors with an Excell file where additional information about e.g. climate and vegetation of the site can be filled in.