Abstract

Climate change is rapidly warming high latitude and high elevation regions influencing plant community composition. Changes in vegetation composition have motivated the coordination of ecological monitoring networks across the Arctic, including the International Tundra Experiment. We have established a long-term passive warming experiment using open-top chambers, which includes five distinct plant communities (Dry Heath; Tussock Tundra; and Dry, Mesic, and Wet Meadow). We measured changes in plant community composition based on relative abundance differences over 26 years. In addition, relative abundance changes in response to fertilization and warming treatments were analyzed based on a seven-year Community-Level Interaction Program experiment. The communities had distinct soil moisture conditions, leading to community-specific responses of the plant growth forms (deciduous shrubs, evergreen shrubs, forbs, and graminoids). Warming significantly affected growth forms, but the direction of the response was not consistent across the communities. Evidence of shrub expansion was found in nearly all communities, with soil moisture determining whether it was driven by deciduous or evergreen shrubs. Graminoids increased in relative abundance in the Dry Meadow due to warming. Growth form responses to warming are likely mediated by edaphic characteristics of the communities and their interactions with climate.

Highlights

  • Climate change is causing drastic changes to the world’s biomes, typically associated with rising global air temperatures

  • We address the effects of passive warming on local patterns in plant community structure over a 26-year period

  • In the International Tundra Experiment (ITEX) experiment, we investigated the effect of passive warming on plant relative abundance through time in the five plant communities

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Summary

Introduction

Climate change is causing drastic changes to the world’s biomes, typically associated with rising global air temperatures. This is especially pronounced in the Arctic and high altitude environments where the temperature has been rising at approximately twice the rate of the global average (Meredith et al 2019). Changes in tundra plant abundance and diversity can have a variety of consequences at both local and global scales. The increase towards taller, more productive vegetation in the tundra can affect climate through its effect on carbon storage and surface albedo (Myers-Smith et al 2011; Post et al 2019). Investigating the effects of warming due to climate change on this sensitive biome was one of the primary motivations for the founding of the International Tundra Experiment (ITEX)

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