Namib Desert primary productivity is driven by cryptic microbial community N-fixation

Abstract Carbon exchange in drylands is typically low, but during significant rainfall events (wet anomalies) drylands act as a C sink. During these anomalies the limitation on C uptake switches from water to nitrogen. In the Namib Desert of southern Africa, the N inventory in soil organic matter av...

Full description

Bibliographic Details
Main Authors: Jean-Baptiste Ramond, Stephan Woodborne, Grant Hall, Mary Seely, Don A. Cowan
Format: Article
Language:English
Published: Nature Publishing Group 2018-05-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-018-25078-4
id doaj-20ba7ddacc0d4eb5afdefd7c70bd76bf
record_format Article
spelling doaj-20ba7ddacc0d4eb5afdefd7c70bd76bf2020-12-08T06:12:05ZengNature Publishing GroupScientific Reports2045-23222018-05-01811910.1038/s41598-018-25078-4Namib Desert primary productivity is driven by cryptic microbial community N-fixationJean-Baptiste Ramond0Stephan Woodborne1Grant Hall2Mary Seely3Don A. Cowan4Department of Biochemistry, Genetics and Microbiology, Centre for Microbial Ecology and Genomics (CMEG), Genomics Research Institute (GRI), University of PretoriaMammal Research Institute, University of PretoriaMammal Research Institute, University of PretoriaGobabeb Research and Training CentreDepartment of Biochemistry, Genetics and Microbiology, Centre for Microbial Ecology and Genomics (CMEG), Genomics Research Institute (GRI), University of PretoriaAbstract Carbon exchange in drylands is typically low, but during significant rainfall events (wet anomalies) drylands act as a C sink. During these anomalies the limitation on C uptake switches from water to nitrogen. In the Namib Desert of southern Africa, the N inventory in soil organic matter available for mineralisation is insufficient to support the observed increase in primary productivity. The C4 grasses that flourish after rainfall events are not capable of N fixation, and so there is no clear mechanism for adequate N fixation in dryland ecosystems to support rapid C uptake. Here we demonstrate that N fixation by photoautotrophic hypolithic communities forms the basis for the N budget for plant productivity events in the Namib Desert. Stable N isotope (δ 15N) values of Namib Desert hypolithic biomass, and surface and subsurface soils were measured over 3 years across dune and gravel plain biotopes. Hypoliths showed significantly higher biomass and lower δ 15N values than soil organic matter. The δ 15N values of hypoliths approach the theoretical values for nitrogen fixation. Our results are strongly indicative that hypolithic communities are the foundation of productivity after rain events in the Namib Desert and are likely to play similar roles in other arid environments.https://doi.org/10.1038/s41598-018-25078-4
collection DOAJ
language English
format Article
sources DOAJ
author Jean-Baptiste Ramond
Stephan Woodborne
Grant Hall
Mary Seely
Don A. Cowan
spellingShingle Jean-Baptiste Ramond
Stephan Woodborne
Grant Hall
Mary Seely
Don A. Cowan
Namib Desert primary productivity is driven by cryptic microbial community N-fixation
Scientific Reports
author_facet Jean-Baptiste Ramond
Stephan Woodborne
Grant Hall
Mary Seely
Don A. Cowan
author_sort Jean-Baptiste Ramond
title Namib Desert primary productivity is driven by cryptic microbial community N-fixation
title_short Namib Desert primary productivity is driven by cryptic microbial community N-fixation
title_full Namib Desert primary productivity is driven by cryptic microbial community N-fixation
title_fullStr Namib Desert primary productivity is driven by cryptic microbial community N-fixation
title_full_unstemmed Namib Desert primary productivity is driven by cryptic microbial community N-fixation
title_sort namib desert primary productivity is driven by cryptic microbial community n-fixation
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2018-05-01
description Abstract Carbon exchange in drylands is typically low, but during significant rainfall events (wet anomalies) drylands act as a C sink. During these anomalies the limitation on C uptake switches from water to nitrogen. In the Namib Desert of southern Africa, the N inventory in soil organic matter available for mineralisation is insufficient to support the observed increase in primary productivity. The C4 grasses that flourish after rainfall events are not capable of N fixation, and so there is no clear mechanism for adequate N fixation in dryland ecosystems to support rapid C uptake. Here we demonstrate that N fixation by photoautotrophic hypolithic communities forms the basis for the N budget for plant productivity events in the Namib Desert. Stable N isotope (δ 15N) values of Namib Desert hypolithic biomass, and surface and subsurface soils were measured over 3 years across dune and gravel plain biotopes. Hypoliths showed significantly higher biomass and lower δ 15N values than soil organic matter. The δ 15N values of hypoliths approach the theoretical values for nitrogen fixation. Our results are strongly indicative that hypolithic communities are the foundation of productivity after rain events in the Namib Desert and are likely to play similar roles in other arid environments.
url https://doi.org/10.1038/s41598-018-25078-4
work_keys_str_mv AT jeanbaptisteramond namibdesertprimaryproductivityisdrivenbycrypticmicrobialcommunitynfixation
AT stephanwoodborne namibdesertprimaryproductivityisdrivenbycrypticmicrobialcommunitynfixation
AT granthall namibdesertprimaryproductivityisdrivenbycrypticmicrobialcommunitynfixation
AT maryseely namibdesertprimaryproductivityisdrivenbycrypticmicrobialcommunitynfixation
AT donacowan namibdesertprimaryproductivityisdrivenbycrypticmicrobialcommunitynfixation
_version_ 1724391371908841472