Biology subjects

Bowman, J. S.

Publications and source records attributed to Bowman, J. S..

3 recordsLinked to original sources

bioRxiv2026

Alkaline phosphatase activity supports heterotrophic carbon acquisition in a coastal time series site and a representative marine bacterium

Phosphorus is a vital nutrient required for the functioning of living organisms. In aquatic environments, dissolved inorganic phosphate is considered its most bioavailable form. However, phosphate can be scarce, which has the potential to limit microbial metabolism and ecosystem functioning. To overcome phosphate scarcity, microbes produce alkaline phosphatase (AP) to access dissolved organic phosphorus (DOP). Here, we conducted a year-long study of alkaline phosphatase activity (APA) at the Ellen Browning Scripps Memorial Pier, a nutrient-rich coastal site. APA was observed throughout the year despite phosphate-replete conditions, suggesting that the role of APs in microbial nutrition is not completely understood. We tested the hypothesis that APA may promote acquisition of organic carbon liberated from DOP hydrolysis by growing the heterotrophic marine bacterium Ruegeria pomeroyi on three DOP compounds as sole carbon sources and assessing APA. Controlling for carbon concentration, all DOP sources supported growth, but at lower levels than glucose, with the highest growth observed on glucose-6-phosphate (G6P), followed by adenosine monophosphate (AMP) and adenosine triphosphate (ATP). Moreover, cell-specific APA was significantly enhanced in carbon-deplete conditions and during growth on G6P, relative to cultures grown on replete glucose or nucleotides. These findings suggest alkaline phosphatases (APs) are part of a generic carbon stress response and likely play a role in acquiring certain forms of organic carbon by R. pomeroyi, with implications for other taxa. Overall, this study helps advance the current state of knowledge regarding microbial phosphorus cycling and carbon utilization in aquatic environments.

microbiology↗

bioRxiv2026

Anaerobic methane oxidation by ANME-2a at two molar chloride in Orca Basin

Anaerobic methane oxidation, typically mediated by consortia of archaea and bacteria, is a key process in the global methane cycle, but little is known about its upper salinity limits. We characterized the microbial methane cycle in the anoxic, hypersaline Orca Basin using metagenomics, metatranscriptomics, fluorescence in situ hybridization, and geochemical measurements at sub-meter resolution. In the brine, we detected transcriptional activity of the halophilic methylotrophic methanogen Methanohalophilus, consistent with a biological source for Orca Basin methane. In the particle-rich halocline ([~]2 M Cl-; [~]2235 meters depth), high mcrA transcription by a novel ANME-2a species was co-located with a positive shift in {delta}13C-CH4 indicative of anaerobic oxidation of methane. ANME-2a also transcribed genes for biosynthesis of the osmolyte N({varepsilon})-acetyl-{beta}-L-lysine, supporting adaptation for hypersaline conditions. At the same depth, consortia of sarcina-like archaea, likely ANME-2a, were observed in association with vibrioid and filamentous bacteria, potentially members of a halotolerant genus in the order Desulfobulbales (family SURF-16, which includes the previously identified ANME partner Seep-DBB) that were active at the same depth. At and above the oxic-anoxic interface, aerobic methane oxidation appears to be mediated by three genera of uncultivated Methylococcales bacteria. Our results double the upper salinity range of ANME-2a to [~]2 M Cl- and reveal the key microbial players in the methane bio-filter between the Orca Basin brine and overlying seawater.

microbiology↗

bioRxiv2026

Assessing climate adaptation among Canada lynx (Lynx canadensis) populations at the trailing edge

Species must acclimate, shift their distributions, or adapt in place in response to anthropogenic climate change. Populations at low-latitude trailing edges of species distributions typically experience thermal conditions closest to the upper limit of their thermoregulatory capacity. Landscape and functional genomic approaches provide quantitative measures of risk and adaptive capacity which can inform and prioritize conservation actions. Using low-coverage whole genomes from Canada lynx (Lynx canadensis), we characterized population genomic structure and identified putatively adaptive loci using genotype-environment association analyses across the eastern extent of their distribution. We detected genetic breaks across two previously identified biogeographical barriers, the St. Lawrence River and the Strait of Belle Isle, and found relatively high genome-wide diversity in the Maine population at the southern trailing edge, suggesting a reservoir of warm-adapted variation. We identified 759 loci from 329 genes as putatively adaptive, many associated with temperature during warm and dry periods, and functionally enriched in photoreception, circadian entrainment, and temperature regulation. We identified ten putatively adaptive genes linked to epilepsy, presenting candidate genes underlying reports of idiopathic epilepsy in captive populations of closely related lynx species (L. lynx and L. pardinus). Genetic offset showed lynx in Western Newfoundland, and the Gaspe Peninsula in Quebec are at the greatest risk of maladaptation under future conditions. If gene flow allows, introgression of climate-adapted loci from the trailing-edge may benefit regional populations under future climates. Together, these findings demonstrate the conservation value of locally adapted range-edge populations.

genomics↗