4.1 Article

The productivity, metabolism and carbon cycle of two lowland tropical forest plots in south-western Amazonia, Peru

Journal

PLANT ECOLOGY & DIVERSITY
Volume 7, Issue 1-2, Pages 85-105

Publisher

TAYLOR & FRANCIS LTD
DOI: 10.1080/17550874.2013.820805

Keywords

allocation; GPP; herbivory; NPP; phenology; seasonality; soil respiration; stem respiration; tropical forests; western Amazonia

Categories

Funding

  1. Gordon and Betty Moore Foundation
  2. UK Natural Environment Research Council [NE/D01025X/1, NE/D014174/1, NE/F002149/1]
  3. NERC AMAZONICA consortium grant
  4. Jackson Foundation
  5. Oxford Martin School
  6. European Research Council Advanced Investigator Grant
  7. NERC [NE/D01185X/1, NE/D010306/1, NE/G018278/1, NE/J023418/1, NE/F002149/1, NE/D011191/1, NE/F005776/1, NE/I02982X/1, NE/D01025X/1, NE/J023531/1, NE/D014174/1] Funding Source: UKRI
  8. Natural Environment Research Council [NE/D011191/1, NE/I02982X/1, NE/D014174/1, NE/B504630/1, NE/J023418/1, NE/G018278/1, NE/J023531/1, NE/F005776/1, NE/D01185X/1, NER/A/S/2003/00608/2, NE/D01025X/1, NE/D010306/1, NE/F002149/1] Funding Source: researchfish

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Background: The forests of western Amazonia are known to be more dynamic that the better-studied forests of eastern Amazonia, but there has been no comprehensive description of the carbon cycle of a western Amazonian forest. Aims: We present the carbon budget of two forest plots in Tambopata in south-eastern Peru, western Amazonia. In particular, we present, for the first time, the seasonal variation in the detailed carbon budget of a tropical forest. Methods: We measured the major components of net primary production (NPP) and total autotrophic respiration over 3-6 years. Results: The NPP for the two plots was 15.1 +/- 0.8 and 14.2 +/- 1.0 Mg C ha(-1) year(-1), the gross primary productivity (GPP) was 35.5 +/- 3.6 and 34.5 +/- 3.5 Mg C ha(-1) year(-1), and the carbon use efficiency (CUE) was 0.42 +/- 0.05 and 0.41 +/- 0.05. NPP and CUE showed a large degree of seasonality. Conclusions: The two plots were similar in carbon cycling characteristics despite the different soils, the most notable difference being high allocation of NPP to canopy and low allocation to fine roots in the Holocene floodplain plot. The timing of the minima in the wet-dry transition suggests they are driven by phenological rhythms rather than being driven directly by water stress. When compared with results from forests on infertile forests in humid lowland eastern Amazonia, the plots have slightly higher GPP, but similar patterns of CUE and carbon allocation.

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