Abstract

Rapidly expanding conversion of tropical forests to oil palm plantations in Southeast Asia leads to soil acidification following intensive nitrogen fertilization. Changes in soil pH are predicted to have an impact on archaeal ammonia-oxidizing archaea (AOA), ammonia-oxidizing bacteria (AOB), and complete (comammox) ammonia oxidizers and, consequently, on nitrification. It is therefore critical to determine whether the predicted effects of pH on ammonia oxidizers and nitrification activity apply in tropical soils subjected to various degrees of anthropogenic activity. This was investigated by experimental manipulation of pH in soil microcosms from a land-use gradient (forest, riparian, and oil palm soils). The nitrification rate was greater in forest soils with native neutral pH than in converted acidic oil palm soils. Ammonia oxidizer activity decreased following acidification of the forest soils but increased after liming of the oil palm soils, leading to a trend of a reversed net nitrification rate after pH modification. AOA and AOB nitrification activity was dependent on pH, but AOB were more sensitive to pH modification than AOA, which demonstrates a greater stability of AOA than AOB under conditions of short-term perturbation. In addition, these results predict AOB to be a good bioindicator of nitrification response following pH perturbation during land-use conversion. AOB and/or comammox species were active in all soils along the land-use gradient, even, unexpectedly, under acidic conditions, suggesting their adaptation to native acidic or acidified soils. The present study therefore provided evidence for limited stability of soil ammonia oxidizer activity following intensive anthropogenic activities, which likely aggravates the vulnerability of nitrogen cycle processes to environmental disturbance.IMPORTANCE Physiological and ecological studies have provided evidence for pH-driven niche specialization of ammonia oxidizers in terrestrial ecosystems. However, the functional stability of ammonia oxidizers following pH change has not been investigated, despite its importance in understanding the maintenance of ecosystem processes following environmental perturbation. This is particularly true after anthropogenic perturbation, such as the conversion of tropical forest to oil palm plantations. This study demonstrated a great impact of land-use conversion on nitrification, which is linked to changes in soil pH due to common agricultural practices (intensive fertilization). In addition, the different communities of ammonia oxidizers were differently affected by short-term pH perturbations, with implications for future land-use conversions but also for increased knowledge of associated global nitrous oxide emissions and current climate change concerns.

Highlights

  • Expanding conversion of tropical forests to oil palm plantations in Southeast Asia leads to soil acidification following intensive nitrogen fertilization

  • Nitrification rates are traditionally considered to be lower in acid soils, due to reduced ammonia availability through ionization of ammonia to ammonium [24], the net nitrification rate does not show a strong relationship with soil pH [25], and this can be explained by the distribution and activities of physiologically diverse groups of ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB) across a range of pH and ecosystems [15, 26, 27]

  • Little is known of the stability of ammonia oxidizer communities following changes in soil pH, despite its ecological importance. pH niche specialization of AOA and AOB suggests that AOA communities are active under a wider range of soil pH than AOB, while evidence for growth of acid-adapted AOB remains scarce [24, 36, 37]

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Summary

Introduction

Expanding conversion of tropical forests to oil palm plantations in Southeast Asia leads to soil acidification following intensive nitrogen fertilization. The functional stability of ammonia oxidizers following pH change has not been investigated, despite its importance in understanding the maintenance of ecosystem processes following environmental perturbation This is true after anthropogenic perturbation, such as the conversion of tropical forest to oil palm plantations. Global oil palm cultivation increased from 3.6 to 19 million ha during the period 1961 to 2018, 63% of which is in Malaysia and Indonesia (FAO, 2018; http://www.fao.org/faostat/en/#data/ QC) This land-use conversion process is marked by intense anthropogenic disturbance, including land clearing, soil drainage, road/track building, seedling plantations, and follow-up agricultural management [3], which impose a major threat to the biodiversity of native tropical forests [4,5,6]. One can presume that AOA populations are more stable than AOB following a decrease in pH, with msystems.asm.org 2

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