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Arctic soil microbial communities may shift with increasing temperatures and water availability from climate change. We examined temperature and volumetric liquid water content (VWC) in the upper 80 cm of permafrost-affected soil over 2 years (2018-2019) at the Bayelva monitoring station, Ny Ålesund, Svalbard. We show VWC increases with depth, whereas in situ temperature is more stable vertically, ranging from -5°C to 5 °C seasonally. Prokaryotic metagenome-assembled genomes (MAGs) were obtained at 2-4 cm vertical resolution collected while frozen in April 2018 and at 10 cm vertical resolution collected while thawed in September 2019. The most abundant MAGs were Acidobacteriota, Actinomycetota, and Chloroflexota. Actinomycetota and Chloroflexota increase with depth, while Acidobacteriota classes Thermoanaerobaculia Gp7-AA8, Blastocatellia UBA7656, and Vicinamibacteria Vicinamibacterales are found above 6 cm, below 6 cm, and below 20 cm, respectively. All MAGs have diverse carbon-degrading genes, and Actinomycetota and Chloroflexota have autotrophic genes. Genes encoding β -glucosidase, N-acetyl-β-D-glucosaminidase, and xylosidase increase with depth, indicating a greater potential for organic matter degradation with higher VWC. Acidobacteriota dominate the top 6 cm with their classes segregating by depth, whereas Actinomycetota and Chloroflexota dominate below ∼6 cm. This suggests that Acidobacteriota classes adapt to lower VWC at the surface, while Actinomycetota and Chloroflexota persist below 6 cm with higher VWC. This indicates that VWC may be as important as temperature in microbial climate change responses in Arctic mineral soils. Here we describe MAG-based Seqcode type species in the Acidobacteriota, Onstottus arcticum, Onstottus frigus, and Gilichinskyi gelida and in the Actinobacteriota, Mayfieldus profundus., Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2024. Published by Elsevier GmbH.)

Background: Dark pigmented snow and glacier ice algae on glaciers and ice sheets contribute to accelerating melt. The biological controls on these algae, particularly the role of viruses, remain poorly understood. Giant viruses, classified under the nucleocytoplasmic large DNA viruses (NCLDV) supergroup (phylum Nucleocytoviricota), are diverse and globally distributed. NCLDVs are known to infect eukaryotic cells in marine and freshwater environments, providing a biological control on the algal population in these ecosystems. However, there is very limited information on the diversity and ecosystem function of NCLDVs in terrestrial icy habitats., Results: In this study, we investigate for the first time giant viruses and their host connections on ice and snow habitats, such as cryoconite, dark ice, ice core, red and green snow, and genomic assemblies of five cultivated Chlorophyta snow algae. Giant virus marker genes were present in almost all samples; the highest abundances were recovered from red snow and the snow algae genomic assemblies, followed by green snow and dark ice. The variety of active algae and protists in these GrIS habitats containing NCLDV marker genes suggests that infection can occur on a range of eukaryotic hosts. Metagenomic data from red and green snow contained evidence of giant virus metagenome-assembled genomes from the orders Imitervirales, Asfuvirales, and Algavirales., Conclusion: Our study highlights NCLDV family signatures in snow and ice samples from the Greenland ice sheet. Giant virus metagenome-assembled genomes (GVMAGs) were found in red snow samples, and related NCLDV marker genes were identified for the first time in snow algal culture genomic assemblies; implying a relationship between the NCLDVs and snow algae. Metatranscriptomic viral genes also aligned with metagenomic sequences, suggesting that NCLDVs are an active component of the microbial community and are potential "top-down" controls of the eukaryotic algal and protistan members. This study reveals the unprecedented presence of a diverse community of NCLDVs in a variety of glacial habitats dominated by algae., (© 2024. The Author(s).)

High-elevation arid regions harbor microbial communities reliant on metabolic niches and flexibility to survive under biologically stressful conditions, including nutrient limitation that necessitates the utilization of atmospheric trace gases as electron donors. Geothermal springs present "oases" of microbial activity, diversity, and abundance by delivering water and substrates, including reduced gases. However, it is unknown whether these springs exhibit a gradient of effects, increasing their impact on trace gas-oxidizers in the surrounding soils. We assessed whether proximity to Polloquere, a high-altitude geothermal spring in an Andean salt flat, alters the diversity and metabolic structure of nearby soil bacterial populations compared to the surrounding cold desert. Recovered DNA and metagenomic analyses indicate that the spring represents an oasis for microbes in this challenging environment, supporting greater biomass with more diverse metabolic functions in proximal soils that declines sharply with radial distance from the spring. Despite the sharp decrease in biomass, potential rates of atmospheric hydrogen (H2) and carbon monoxide (CO) uptake increase away from the spring. Kinetic estimates suggest this activity is due to high-affinity trace gas consumption, likely as a survival strategy for energy/carbon acquisition. These results demonstrate that Polloquere regulates a gradient of diverse microbial communities and metabolisms, culminating in increased activity of trace gas-oxidizers as the influence of the spring yields to that of the regional salt flat environment. This suggests the spring holds local importance within the context of the broader salt flat and potentially represents a model ecosystem for other geothermal systems in high-altitude desert environments., (© The Author(s) 2024. Published by Oxford University Press on behalf of the International Society for Microbial Ecology.)

The Greenland Ice Sheet is a biome which is mainly microbially driven. Several different niches can be found within the glacial biome for those microbes able to withstand the harsh conditions, e.g., low temperatures, low nutrient conditions, high UV radiation in summer, and contrasting long and dark winters. Eukaryotic algae can form blooms during the summer on the ice surface, interacting with communities of bacteria, fungi, and viruses. Cryoconite holes and snow are also habitats with their own microbial community. Nevertheless, the microbiome of supraglacial habitats remains poorly studied, leading to a lack of representative genomes from these environments. Under-investigated extremophiles, like those living on the Greenland Ice Sheet, may provide an untapped reservoir of chemical diversity that is yet to be discovered. In this study, an inventory of the biosynthetic potential of these organisms is made, through cataloging the presence of biosynthetic gene clusters in their genomes. There were 133 high-quality metagenome-assembled genomes (MAGs) and 28 whole genomes of bacteria obtained from samples of the ice sheet surface, cryoconite, biofilm, and snow using culturing-dependent and -independent approaches. AntiSMASH and BiG-SCAPE were used to mine these genomes and subsequently analyze the resulting predicted gene clusters. Extensive sets of predicted Biosynthetic Gene Clusters (BGCs) were collected from the genome collection, with limited overlap between isolates and MAGs. Additionally, little overlap was found in the biosynthetic potential among different environments, suggesting specialization of organisms in specific habitats. The median number of BGCs per genome was significantly higher for the isolates compared to the MAGs. The most talented producers were found among Proteobacteria. We found evidence for the capacity of these microbes to produce antimicrobials, carotenoid pigments, siderophores, and osmoprotectants, indicating potential survival mechanisms to cope with extreme conditions. The majority of identified BGCs, including those in the most prevalent gene cluster families, have unknown functions, presenting a substantial potential for bioprospecting. This study underscores the diverse biosynthetic potential in Greenland Ice Sheet genomes, revealing insights into survival strategies and highlighting the need for further exploration and characterization of these untapped resources., Competing Interests: The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest. The author(s) declared that they were an editorial board member of Frontiers, at the time of submission. This had no impact on the peer review process and the final decision., (Copyright © 2023 Jaarsma, Zervas, Sipes, Campuzano Jiménez, Smith, Svendsen, Thøgersen, Stougaard, Benning, Tranter and Anesio.)

The microbiome of Greenland Ice Sheet supraglacial habitats is still underinvestigated, and as a result there is a lack of representative genomes from these environments. In this study, we investigated the supraglacial microbiome through a combination of culturing-dependent and -independent approaches. We explored ice, cryoconite, biofilm, and snow biodiversity to answer: (1) how microbial diversity differs between supraglacial habitats, (2) if obtained bacterial genomes reflect dominant community members, and (3) how culturing versus high throughput sequencing changes our observations of microbial diversity in supraglacial habitats. Genomes acquired through metagenomic sequencing (133 high-quality MAGs) and whole genome sequencing (73 bacterial isolates) were compared to the metagenome assemblies to investigate abundance within the total environmental DNA. Isolates obtained in this study were not dominant taxa in the habitat they were sampled from, in contrast to the obtained MAGs. We demonstrate here the advantages of using metagenome SSU rRNA genes to reflect whole-community diversity. Additionally, we demonstrate a proof-of-concept of the application of in situ culturing in a supraglacial setting., (© The Author(s) 2023. Published by Oxford University Press on behalf of FEMS.)

Ten distinct isolates from the genus Pseudomonas were isolated in culture. The genomes of these isolates were sequenced using the Illumina MiSeq platform and assembled in order to provide insight into the metabolic and carbon-degrading potential of bacteria residing in soils at high latitudes.

As marine sediments are buried, microbial communities transition from sulfate-reduction to methane-production after sulfate is depleted. When this biogenic methane diffuses into the overlying sulfate-rich sediments, it forms a sulfate-methane transition zone (SMTZ) because sulfate reducers deplete hydrogen concentrations and make hydrogenotrophic methanogenesis exergonic in the reverse direction, a process called the anaerobic oxidation of methane (AOM). Microbial participation in these processes is often inferred from geochemistry, genes, and gene expression changes with sediment depth, using sedimentation rates to convert depth to time. Less is known about how natural sediments transition through these geochemical states transition in real-time. We examined 16S rRNA gene amplicon libraries and metatranscriptomes in microcosms of anoxic sediment from the White Oak River estuary, NC, with three destructively sampled replicates with methane added (586-day incubations) and three re-sampled un-amended replicates (895-day incubations). Sulfate dropped to a low value (∼0.3 mM) on similar days for both experiments (312 and 320 days, respectively), followed by a peak in hydrogen, intermittent increases in methane-cycling archaea starting on days 375 and 362 (mostly Methanolinea spp. and Methanosaeta spp., and Methanococcoides sp. ANME-3), and a methane peak 1 month later. However, methane δ 13 C values only show net methanogenesis 6 months after methane-cycling archaea increase and 4 months after the methane peak, when sulfate is consistently below 0.1 mM and hydrogen increases to a stable 0.61 ± 0.13 nM (days 553-586, n = 9). Sulfate-reducing bacteria (mostly Desulfatiglans spp. and Desulfosarcina sp. SEEP-SRB1) increase in relative abundance only during this period of net methane production, suggesting syntrophy with methanogens in the absence of sulfate. The transition from sulfate reduction to methane production in marine sediments occurs through a prolonged period of methane-cycling by methanogens at low sulfate concentrations, and steady growth of sulfate reducers along with methanogens after sulfate is depleted., Competing Interests: The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest., (Copyright © 2022 Kevorkian, Sipes, Winstead, Paul and Lloyd.)

The active layer of permafrost in Ny Ålesund, Svalbard (79°N) around the Bayelva River in the Leirhaugen glacier moraine is measured as a small net carbon sink at the brink of becoming a carbon source. In many permafrost-dominating ecosystems, microbes in the active layers have been shown to drive organic matter degradation and greenhouse gas production, creating positive feedback on climate change. However, the microbial metabolisms linking the environmental geochemical processes and the populations that perform them have not been fully characterized. In this paper, we present geochemical, enzymatic, and isotopic data paired with 10 Pseudomonas sp. cultures and metagenomic libraries of two active layer soil cores (BPF1 and BPF2) from Ny Ålesund, Svalbard, (79°N). Relative to BPF1, BPF2 had statistically higher C/N ratios (15 ± 1 for BPF1 vs. 29 ± 10 for BPF2; n = 30, p < 10 -5 ), statistically lower organic carbon (2% ± 0.6% for BPF1 vs. 1.6% ± 0.4% for BPF2, p < 0.02), statistically lower nitrogen (0.1% ± 0.03% for BPF1 vs. 0.07% ± 0.02% for BPF2, p < 10 -6 ). The d 13 C values for inorganic carbon did not correlate with those of organic carbon in BPF2, suggesting lower heterotrophic respiration. An increase in the δ 13 C of inorganic carbon with depth either reflects an autotrophic signal or mixing between a heterotrophic source at the surface and a lithotrophic source at depth. Potential enzyme activity of xylosidase and N-acetyl-β-D-glucosaminidase increases twofold at 15°C, relative to 25°C, indicating cold adaptation in the cultures and bulk soil. Potential enzyme activity of leucine aminopeptidase across soils and cultures was two orders of magnitude higher than other tested enzymes, implying that organisms use leucine as a nitrogen and carbon source in this nutrient-limited environment. Besides demonstrating large variability in carbon compositions of permafrost active layer soils only ∼84 m apart, results suggest that the Svalbard active layer microbes are often limited by organic carbon or nitrogen availability and have adaptations to the current environment, and metabolic flexibility to adapt to the warming climate., Competing Interests: The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest., (Copyright © 2022 Sipes, Paul, Fine, Li, Liang, Boike, Onstott, Vishnivetskaya, Schaeffer and Lloyd.)

Permafrost microbes may be metabolically active in microscopic layers of liquid brines, even in ancient soil. Metagenomics can help discern whether permafrost microbes show adaptations to this environment. Thirty-three metagenome-assembled genomes (MAGs) were obtained from six depths (3.5 m to 20 m) of freshly cored permafrost from the Siberian Kolyma-Indigirka Lowland region. These soils have been continuously frozen for ∼20,000 to 1,000,000 years. Eight of these MAGs were ≥80% complete with <10% contamination and were taxonomically identified as Aminicenantes , Atribacteria , Chloroflexi , and Actinobacteria within bacteria and Thermoprofundales within archaea. MAGs from these taxa have been obtained previously from nonpermafrost environments and have been suggested to show adaptations to long-term energy starvation, but they have never been explored in ancient permafrost. The permafrost MAGs had greater proportions in the Clusters of Orthologous Groups (COGs) categories of energy production and conversion and carbohydrate transport and metabolism than did their nonpermafrost counterparts. They also contained genes for trehalose synthesis, thymine metabolism, mevalonate biosynthesis, and cellulose degradation, which were less prevalent in nonpermafrost genomes. Many of these genes are involved in membrane stabilization and osmotic stress responses, consistent with adaptation to the anoxic, high-ionic-strength, cold environments of permafrost brine films. Our results suggest that this ancient permafrost contains DNA of high enough quality to assemble MAGs from microorganisms with adaptations to survive long-term freezing in this extreme environment. IMPORTANCE Permafrost around the world is thawing rapidly. Many scientists from a variety of disciplines have shown the importance of understanding what will happen to our ecosystem, commerce, and climate when permafrost thaws. The fate of permafrost microorganisms is connected to these predicted rapid environmental changes. Studying ancient permafrost with culture-independent techniques can give a glimpse into how these microorganisms function under these extreme low-temperature and low-energy conditions. This will facilitate understanding how they will change with the environment. This study presents genomic data from this unique environment ∼20,000 to 1,000,000 years of age.

Distinct lineages of Gammaproteobacteria clade Woeseiales are globally distributed in marine sediments, based on metagenomic and 16S rRNA gene analysis. Yet little is known about why they are dominant or their ecological role in Arctic fjord sediments, where glacial retreat is rapidly imposing change. This study combined 16S rRNA gene analysis, metagenome-assembled genomes (MAGs), and genome-resolved metatranscriptomics uncovered the in situ abundance and transcriptional activity of Woeseiales with burial in four shallow sediment sites of Kongsfjorden and Van Keulenfjorden of Svalbard (79°N). We present five novel Woeseiales MAGs and show transcriptional evidence for metabolic plasticity during burial, including sulfur oxidation with reverse dissimilatory sulfite reductase (dsrAB) down to 4 cm depth and nitrite reduction down to 6 cm depth. A single stress protein, spore protein SP21 (hspA), had a tenfold higher mRNA abundance than any other transcript, and was a hundredfold higher on average than other transcripts. At three out of the four sites, SP21 transcript abundance increased with depth, while total mRNA abundance and richness decreased, indicating a shift in investment from metabolism and other cellular processes to build-up of spore protein SP21. The SP21 gene in MAGs was often flanked by genes involved in membrane-associated stress response. The ability of Woeseiales to shift from sulfur oxidation to nitrite reduction with burial into marine sediments with decreasing access to overlying oxic bottom waters, as well as enter into a dormant state dominated by SP21, may account for its ubiquity and high abundance in marine sediments worldwide, including those of the rapidly shifting Arctic., Competing Interests: The authors have declared that no competing interests exist.

Background: Chronic Kidney Disease (CKD) is associated with alterations in phosphorus excretion, and increases in fibroblast growth factor (FGF23) and parathyroid hormone (PTH). Plant protein-based phytate-bound phosphorus, is less bioavailable than that from animal sources. Our one-week study that was conducted previously showed that a nearly 100% plant protein-based diet benefits mineral metabolism in CKD; however, this diet may not be acceptable to patients. Here we hypothesize that a diet containing 70% protein from plants has similar efficacy and is tolerated by CKD patients., Methods: Thirteen subjects with CKD 3-4 received an omnivorous diet containing 70% protein from plants for 4 weeks. The primary outcome was change in 24 h urine phosphorus. Secondary outcomes were changes in serum phosphorus, FGF23, PTH, urine sodium excretion, grip strength and fat free mass. Repeated measures analysis of variance (ANOVA) was used to test differences in parameters over the 4 weeks., Results: Mean age of subjects was 54.8 years. Median eGFR was 26 (IQR 14.7) ml/min/1.73 m(2). Over the 4-week period, urine phosphorus significantly decreased by 215 ± 232 mg/day (p < 0.001). No significant changes in serum FGF23, phosphorus or PTH were noted. Urine sodium and titratable acid decreased significantly on the diet. Hand grip strength and fat-free mass did not change. There were two hyperkalemia events both 5.8 mEq/l, corrected by food substitutions. No other adverse events were observed., Conclusions: A 70% plant protein diet is safe, tolerated, and efficacious in lowering urine phosphorus excretion and may be an alternative to phosphate binders., (© 2015 S. Karger AG, Basel.)

Objective: To analyze surface antigen expression and functional responses of leukocytes from calves heterozygous and homozygous for bovine leukocyte adhesion deficiency (BLAD)., Animals: 8 clinically normal calves, 4 calves heterozygous for BLAD, and 4 calves homozygous for BLAD., Procedure: Surface antigen expression was examined by flow cytometric analysis of leukocytes stained with monoclonal antibodies. Neutrophil function analyses included phagocytosis and killing of Candida albicans and measurement of respiratory burst activity using cytochrome c and dihydrorhodamine 123 assays. Differential leukocyte counts also were performed., Results: Leukocytes from heterozygous calves were similar to those of clinically normal calves with respect to surface antigen expression, C albicans phagocytosis and killing, and respiratory burst activity. In contrast, neutrophils from calves homozygous for BLAD had significantly reduced phagocytic and yeast-killing capacity but had higher respiratory burst activity than cells from clinically normal or heterozygous calves. Homozygous calves also had extreme neutrophilia and significantly more immature neutrophils., Conclusions: The heterozygous BLAD genotype does not cause detectable functional differences in leukocytes, compared with those of clinically normal calves. In contrast, leukocytes from homozygous calves seem to upregulate alternative host defense capabilities (eg, respiratory burst activity) to partially compensate for the lack of typical adherence-dependent host defense functions.

A prerequisite for studies on bovine neutrophils is a reliable method of neutrophil isolation from blood to obtain highly purified cell populations that are functionally active. Since current techniques of neutrophil isolation fall short of these requirements, we have developed a newer and more effective technique for isolation of bovine neutrophils that utilizes biomagnetic beads coated with a monoclonal antibody that recognizes an abundant surface antigen on bovine neutrophils to purify these cells. Comparison of the purity and viability of bovine neutrophils isolated by a conventional method (continuous Percoll density gradient) with this new method showed that neutrophils isolated with biomagnetic beads were higher in purity and had an increased yield. In addition, cells isolated with biomagnetic beads demonstrated normal or even improved function in assays of chemotaxis, phagocytosis, degranulation, and respiratory burst activity. Finally, bovine neutrophils isolated using this method showed an overall lower level of spontaneous apoptosis, which correlates well with the high level of viability observed in the purified cell preparations. Thus, this method represents a significant advance over current methods for isolating bovine neutrophils and would be widely applicable to labs studying the biochemistry and signal transduction pathways in these cells.

Peroxynitrite is a potent oxidant generated from the reaction of nitric oxide (NO) and superoxide anion (O2-), both of which can be produced in inflammatory tissues. In these studies, we analyzed what direct effect peroxynitrite had on neutrophil (PMN) function. We found that peroxynitrite was an effective priming agent for PMNs, as demonstrated by enhanced O2- production on subsequent activation with low doses of PMA or N-formyl-methionine-leucine-phenylalanine (fMLF), changes in the expression of PMN surface markers (L-selectin, Mac-1, flavocytochrome b, and fMLF receptor), and increased intracellular calcium levels. Analysis of the mechanism of PMN priming by peroxynitrite demonstrated that peroxynitrite resulted in minimal oxidation of protein sulfhydryl groups and subsequent protein cross-linking. In contrast, treatment of PMNs with peroxynitrite resulted in significant nitration of tyrosine residues on neutrophil proteins. In addition, inhibition of tyrosine nitration with a pyrrolopyrimidine antioxidant blocked the majority of peroxynitrite-induced priming effects, further suggesting that PMN priming was mediated primarily by nitration of tyrosine residues on PMN proteins. The ability of peroxynitrite to serve as an effective priming agent for PMNs at sites of inflammation may play a key role in modulating the host-defense process.

We characterized the dose response of bovine neutrophils to platelet-activating factor (PAF) with respect to the following functions: calcium flux and membrane potential changes, actin polymerization, degranulation, and the production and/or priming of the oxidative burst. PAF at very low concentrations (10(-10) and 10(-9) M) caused changes in intracellular calcium and membrane potential in bovine neutrophils, whereas moderate PAF concentrations (> or = 10(-7) M) resulted in increased actin polymerization. Degranulation responses to PAF were more complex: low concentrations (10(-9) M) caused secretory granule degranulation, moderate doses (> or = 10(-7) M) caused specific granule degranulation, whereas azurophil degranulation only occurred at high (10(-5) M) PAF concentrations. Treatment of bovine neutrophils with PAF at concentrations > or = 10(-7) M also caused up-regulation of the adhesion molecules Mac-l and L-selectin. PAF stimulation resulted in a very weak [compared to phorbol myristate acetate (PMA)] oxidative burst in bovine neutrophils, and only at high (10(-6) M) concentrations. Unlike human neutrophils, bovine neutrophils were poorly primed by PAF treatment. Only high concentrations of PAF (10(-5) M) caused an increased rate of PMA-stimulated superoxide production, although lower doses of PAF did reduce the lag time preceding the PMA-induced oxidative burst. The overall pattern that can be inferred is that lower concentrations of PAF promote neutrophil sensitivity and interaction by selective degranulation, up-regulation of adhesion molecules, and increased actin polymerization. In contrast, higher PAF concentrations can promote, albeit weakly, more direct bactericidal responses, such as the release of reactive oxygen species and granule enzymes. The ability of PAF to modulate a graded response in bovine neutrophils would allow the cell to respond proportionally to the severity of a stimulus.

Neutrophils play an essential role in the cellular defense of the bovine mammary gland and compromised leukocyte function has been linked to the development of bovine mastitis. During mastitis, large numbers of leukocytes migrate into the mammary tissues where they become activated, resulting in the assembly of neutrophil membrane and cytosolic proteins to form a superoxide anion-generating complex known as the NADPH oxidase. The key membrane-associated component of the NADPH oxidase is flavocytochrome b, which is a heterodimer of p22-phox and gp91-phox. Currently, only the human, porcine, murine, and rattus p22-phox and the human, porcine, and murine gp91-phox gene sequences are known. Because of the important role neutrophils play in bovine host defense, we carried out studies to clone, sequence, and analyze expression of bovine flavocytochrome b. Using polymerase chain reaction cloning techniques and a bovine spleen cDNA library we have cloned both of the bovine flavocytochrome b subunits, p22-phox and gp91-phox. Comparison of the bovine sequences with those of other species also revealed important information regarding key structural features of gp91-phox and p22-phox, including location of putative glycosylation sites. This study greatly contributes to our understanding of the potential functional sites of the flavocytochrome b subunits as well as providing information that can be used to study the role of neutrophils in bovine inflammatory diseases such as mastitis.

Jacobine (JAC) is a pyrolizidine alkaloid (PA) exhibiting adverse hepatic effects similar to those induced by another PA, monocrotaline (MCT). The in vitro reaction kinetics of JAC, however, have been reported to differ quantitively from those of MCT. We report results of experiments to detect and characterize hepatic DNA damage resulting from in vivo administration of JAC (5-60 mg/kg i.p.) to male Sprague-Dawley rats. Hepatic nuclei were isolated and served as the source of DNA in these experiments. Alkaline elution was employed to characterize the type(s) of DNA damage induced. At 4 h post administration, JAC induced significant dose-dependent DNA-DNA interstrand cross-linking over the entire range of doses. Significant DNA-protein cross-linking was also induced by doses of 15-60 mg/kg. No DNA single-strand breaks were detected. Previous studies in this laboratory have shown MCT to induce these same types of lesions. Results from these experiments demonstrate that despite a reported difference in vitro reaction kinetics, these compounds induce a similar spectrum of DNA damage in the target organ of a susceptible species, where the adverse effects induced are also similar. such similarities are consistent with the involvement of DNA damage in the adverse hepatic effects of PAs.