Abstract

The Tibetan Plateau is highly sensitive to elevated temperatures and has experienced significant climate warming in the last decades. While climate warming is known to greatly impact alpine ecosystems, the gas exchange responses at the leaf and community levels to climate warming in alpine meadow ecosystems remain unclear. In this study, the alpine grass, Elymus nutans, and forb, Potentilla anserina, were grown in open-top chambers (OTCs) for 3 consecutive years to evaluate their response to warming. Gas exchange measurements were used to assess the effects of in-situ warming on leaf- and community-level photosynthetic carbon assimilation based on leaf photosynthetic physiological parameters. We introduced a means of up-scaling photosynthetic measurements from the leaf level to the community level based on six easily measurable parameters, including leaf net photosynthetic rate, fresh leaf mass per unit leaf area, fresh weight of all plant leaves in the community, the percentage of healthy leaves, the percentage of received effective light by leaves in the community, and community coverage. The community-level photosynthetic carbon assimilation and productivity all increased with warming, and the net photosynthetic rate at the leaf level was significantly higher than at the community level. Under elevated temperature, the net photosynthetic rate of E. nutans decreased, while that of P. anserina increased. These results indicated that climate warming may significantly influence plant carbon assimilation, which could alter alpine meadow community composition in the future.

Highlights

  • The global average air temperature has increased continuously since the industrial revolution (IPCC, 2013)

  • The mean ground surface temperatures at 1.5 m during the vigorous growth periods were 14.2 and 13.3◦C in the open-top chambers (OTCs) and Open areas (OAs), and the air temperatures in the OTCs was increased by 0.9◦C (p < 0.05, Table 1)

  • The maximum photosynthetic rate (Pn) for E. nutans and P. anserina occurred at 9:00 AM local time

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Summary

Introduction

The global average air temperature has increased continuously since the industrial revolution (IPCC, 2013). High-latitude and high-altitude ecosystems are exceptionally sensitive to rising temperatures and experience greater increases in amplitude (Yang et al, 2010). The Tibetan Plateau have experienced rapid climate warming (0.4◦C per decade for the past 50 years), exceeding the global mean value, and the warming is expected to increase by 0.6–0.9◦C per decade in the 2015–2050 period (Ma et al, 2017). Climate warming has a significant impact on ecosystem carbon cycles, causing both positive and negative feedbacks to future climates (Brient and Bony, 2013). Alpine meadow is a typical vegetation type in the Tibetan Plateau that is fragile and sensitive to human activities and climate change (Peng et al, 2015).

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