Calcium in the micropylar secretion and receptivity of explanted Crocus ovules to intra- and interspecific pollen

The micropylar secrete of the ovules of Crocus vernus ssp. vernus was analyzed for the Ca⁺² content by atomic absorption, and its capacity to germinate and attract pollen was tested by pollinating explanted ovules, and incubating in absence of culture medium. The results display a Ca⁺² concentration of 28.9 mM in the micropylar secrete. On this secrete both compatible- and incompatible pollen germinates with a mean percentage of 53.7%, and their pollen tubes enter the micropylar canal with percentages of 32.3% to 21.0%. In situ the ovules fail to attract tubes of incompatible pollen. The results are discussed in relation to the ovule receptivity and the guided growth of pollen tubes, substantiating the model of the tropic growth towards increasing calcium concentrations.     

Propagation of viral genomes by replicating ammonia-oxidising archaea during soil nitrification

Ammonia-oxidising archaea (AOA) are a ubiquitous component of microbial communities and dominate the first stage of nitrification in some soils. While we are beginning to understand soil virus dynamics, we have no knowledge of the composition or activity of those infecting nitrifiers or their potential to influence processes. This study aimed to characterise viruses having infected autotrophic AOA in two nitrifying soils of contrasting pH by following transfer of assimilated CO₂-derived ¹³C from host to virus via DNA stable-isotope probing and metagenomic analysis. Incorporation of ¹³C into low GC mol% AOA and virus genomes increased DNA buoyant density in CsCl gradients but resulted in co-migration with dominant non-enriched high GC mol% genomes, reducing sequencing depth and contig assembly. We therefore developed a hybrid approach where AOA and virus genomes were assembled from low buoyant density DNA with subsequent mapping of ¹³C isotopically enriched high buoyant density DNA reads to identify activity of AOA. Metagenome-assembled genomes were different between the two soils and represented a broad diversity of active populations. Sixty-four AOA-infecting viral operational taxonomic units (vOTUs) were identified with no clear relatedness to previously characterised prokaryote viruses. These vOTUs were also distinct between soils, with 42% enriched in ¹³C derived from hosts. The majority were predicted as capable of lysogeny and auxiliary metabolic genes included an AOA-specific multicopper oxidase suggesting infection may augment copper uptake essential for central metabolic functioning. These findings indicate virus infection of AOA may be a frequent process during nitrification with potential to influence host physiology and activity.Subject terms: Microbial ecology, Stable isotope analysis

Microbially mediated oxidation of ammonia to nitrate during nitrification is a central component of the global nitrogen (N) cycle. It is also responsible for major losses of applied fertiliser N in soil, generating atmospheric pollution via direct and indirect production of nitrous oxide (N₂O) as well as nitrate (NO₃^-) pollution of groundwater [1]. Autotrophic ammonia-oxidising archaea (AOA) of the class Nitrososphaeria are a ubiquitous component of soil microbial communities and often dominate ammonia oxidation and nitrification-associated N₂O emissions when ammonia is supplied at low rates via organic matter mineralisation [2], slow-release fertilisers [3] or in acidic soils [4]. Integrated temperate viruses (proviruses) and other virus-associated protein-encoding genes are found in most AOA genomes suggesting frequent interaction (see Supplementary Text). While viruses infecting marine AOA have been characterised through metagenomic approaches [5] and cultivation [6], those infecting soil AOA or other nitrifier groups are currently uncharacterised.Virus infection can influence biogeochemical cycling by augmenting host activity or causing cell mortality and subsequent release of nutrients [7]. Recent advances have demonstrated that soil virus communities are dynamic in a wide range of soils [e.g. 8, 9] and augmenting virus loads modulate C and N fluxes [10, 11]. Nevertheless, identifying active interactions with specific populations or functional groups in soil remains challenging due to structural complexity and the vast diversity of hosts and viruses. Recent use of stable-isotope approaches has investigated whole community host-virus dynamics [12, 13] or interactions between individual host-virus populations specific to a functional process and substrate [14]. The aim of this study was to utilise the latter approach with ¹³CO₂-based DNA-SIP to focus on nitrification-associated interactions and to test the hypothesis that viruses are a dynamic component of soil AOA activity.