Protracted oxygenation across the Cambrian-Ordovician transition: A key initiator of the Great Ordovician Biodiversification Event?

Fluctuations in marine oxygen concentrations have been invoked as a primary driver for changes in biodiversity throughout Earth history. Expansions in reducing marine conditions are commonly invoked as key causal mechanisms for mass extinctions, while increases in marine oxygenation are becoming an increasingly common causal mechanism invoked for biodiversification events. Here we utilize a multiproxy approach to constrain local and global marine paleoredox conditions throughout the late Cambrian-Early Ordovician from two drill core successions in Baltoscandia. Local paleoredox proxies such as manganese concentrations and iron speciation reveal that both sites in the Baltic paleobasin had persistently anoxic and predominantly euxinic (anoxic and sulfidic) bottom water conditions throughout the study interval. Corresponding trace metal datasets indicate nuanced contraction and expansion of global anoxic and euxinic conditions along continental margins during the late Cambrian-Early Ordovician. Lastly, thallium isotope data from these locally reducing sections suggest a global expansion of oxygenated shelf and deeper marine environments from the late Cambrian into the Early Ordovician. This evidence for increasingly oxic marine environments coincides with increases in burrowing depth and tiering in marine animals, as well as diversification of body fossils throughout this ~8-million-year interval. The collective geochemical datasets provide some of the first direct paleoredox evidence for an increase in marine oxygen concentrations as a key mechanism for the Ordovician radiation of marine life.

Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction

The timing and connections between global cooling, marine redox conditions, and biotic turnover are underconstrained for the Late Ordovician. The second most severe mass extinction occurred at the end of the Ordovician period, resulting in ~85% loss of marine species between two extinction pulses. As the only "Big 5" extinction that occurred during icehouse conditions, this interval is an important modern analog to constrain environmental feedbacks. We present a previously unexplored thallium isotope records from two paleobasins that record global marine redox conditions and document two distinct and rapid excursions suggesting vacillating (de)oxygenation. The strong temporal link between these perturbations and extinctions highlights the possibility that dynamic marine oxygen fluctuations, rather than persistent, stable global anoxia, played a major role in driving the extinction. This evidence for rapid oxygen changes leading to mass extinction has important implications for modern deoxygenation and biodiversity declines.

Globally distributed iridium layer preserved within the Chicxulub impact structure

The Cretaceous-Paleogene (K-Pg) mass extinction is marked globally by elevated concentrations of iridium, emplaced by a hypervelocity impact event 66 million years ago. Here, we report new data from four independent laboratories that reveal a positive iridium anomaly within the peak-ring sequence of the Chicxulub impact structure, in drill core recovered by IODP-ICDP Expedition 364. The highest concentration of ultrafine meteoritic matter occurs in the post-impact sediments that cover the crater peak ring, just below the lowermost Danian pelagic limestone. Within years to decades after the impact event, this part of the Chicxulub impact basin returned to a relatively low-energy depositional environment, recording in unprecedented detail the recovery of life during the succeeding millennia. The iridium layer provides a key temporal horizon precisely linking Chicxulub to K-Pg boundary sections worldwide.

Constraining oceanic oxygenation during the Shuram excursion in South China using thallium isotopes

Ediacaran sediments record an unusual global carbon cycle perturbation that has been linked to widespread oceanic oxygenation, the Shuram negative C isotope excursion (NCIE). However, proxy-based estimates of global ocean redox conditions during this event have been limited largely due to proxy specificity (e.g., euxinic sediments for Mo and U isotopes). Modern global seawater documents a homogenous Tl isotope composition (ε²⁰⁵ Tl = -6.0) due to significant manganese oxide burial, which is recorded in modern euxinic sediments. Here, we provide new data documenting that sediments deposited beneath reducing but a non-sulfidic water column from the Santa Barbara Basin (ε²⁰⁵ Tl = -5.6 ± 0.1) also faithfully capture global seawater Tl isotope values. Thus, the proxy utilization of Tl isotopes can extend beyond strictly euxinic settings. Second, to better constrain the global redox conditions during the Shuram NCIE, we measured Tl isotopes of locally euxinic and ferruginous shales of the upper Doushantuo Formation, South China. The ε²⁰⁵ Tl values of these shales exhibit a decreasing trend from ≈-3 to ≈-8, broadly coinciding with the onset of Shuram NCIE. There are ε²⁰⁵ Tl values (-5.1 to -7.8) during the main Shuram NCIE interval that approach values more negative than modern global seawater. These results suggest that manganese oxide burial was near or even greater than modern burial fluxes, which is likely linked to an expansion of oxic conditions. This ocean oxygenation may have been an important trigger for the Shuram NCIE and evolution of Ediacaran-type biota. Subsequently, Tl isotopes show an increasing trend from the modern ocean value to values near the modern global inputs or even heavier (ε²⁰⁵ Tl ≈ -2.5 ~ 0.4), occurring prior to recovery from the NCIE. These records may suggest that there was a decrease in the extent of oxygenated conditions in the global oceans during the late stage of the Shuram NCIE.

Absence of biomarker evidence for early eukaryotic life from the Mesoproterozoic Roper Group: Searching across a marine redox gradient in mid-Proterozoic habitability

By about 2.0 billion years ago (Ga), there is evidence for a period best known for its extended, apparent geochemical stability expressed famously in the carbonate-carbon isotope data. Despite the first appearance and early innovation among eukaryotic organisms, this period is also known for a rarity of eukaryotic fossils and an absence of organic biomarker fingerprints for those organisms, suggesting low diversity and relatively small populations compared to the Neoproterozoic era. Nevertheless, the search for diagnostic biomarkers has not been performed with guidance from paleoenvironmental redox constrains from inorganic geochemistry that should reveal the facies that were most likely hospitable to these organisms. Siltstones and shales obtained from drill core of the ca. 1.3-1.4 Ga Roper Group from the McArthur Basin of northern Australia provide one of our best windows into the mid-Proterozoic redox landscape. The group is well dated and minimally metamorphosed (of oil window maturity), and previous geochemical data suggest a relatively strong connection to the open ocean compared to other mid-Proterozoic records. Here, we present one of the first integrated investigations of Mesoproterozoic biomarker records performed in parallel with established inorganic redox proxy indicators. Results reveal a temporally variable paleoredox structure through the Velkerri Formation as gauged from iron mineral speciation and trace-metal geochemistry, vacillating between oxic and anoxic. Our combined lipid biomarker and inorganic geochemical records indicate at least episodic euxinic conditions sustained predominantly below the photic zone during the deposition of organic-rich shales found in the middle Velkerri Formation. The most striking result is an absence of eukaryotic steranes (4-desmethylsteranes) and only traces of gammacerane in some samples-despite our search across oxic, as well as anoxic, facies that should favor eukaryotic habitability and in low maturity rocks that allow the preservation of biomarker alkanes. The dearth of Mesoproterozoic eukaryotic sterane biomarkers, even within the more oxic facies, is somewhat surprising but suggests that controls such as the long-term nutrient balance and other environmental factors may have throttled the abundances and diversity of early eukaryotic life relative to bacteria within marine microbial communities. Given that molecular clocks predict that sterol synthesis evolved early in eukaryotic history, and (bacterial) fossil steroids have been found previously in 1.64 Ga rocks, then a very low environmental abundance of eukaryotes relative to bacteria is our preferred explanation for the lack of regular steranes and only traces of gammacerane in a few samples. It is also possible that early eukaryotes adapted to Mesoproterozoic marine environments did not make abundant steroid lipids or tetrahymanol in their cell membranes.

Fully oxygenated water columns over continental shelves before the Great Oxidation Event

Late Archaean sedimentary rocks contain compelling geochemical evidence for episodic accumulation of dissolved oxygen in the oceans along continental margins before the Great Oxidation Event. However, the extent of this oxygenation remains poorly constrained. Here we present thallium and molybdenum isotope compositions for anoxic organic-rich shales of the 2.5 billion-year-old Mount McRae Shale from Western Australia, which previously yielded geochemical evidence of a transient oxygenation event. During this event, we observe an anti-correlation between thalium and molybdenum isotope data, including two shifts to higher molybdenum and lower thalium isotope compositions. Our data indicate pronounced burial of manganese oxides in sediments elsewhere in the ocean at these times, which requires that water columns above portions of the ocean floor were fully oxygenated: all the way from the air-sea interface to well below the sediment-water interface. Well-oxygenated continental shelves were likely the most important sites of manganese oxide burial and mass-balance modeling results suggest that fully oxygenated water columns were at least a regional-scale feature of early-Earth's oceans 2.5 billion years ago.

Constraining the rate of oceanic deoxygenation leading up to a Cretaceous Oceanic Anoxic Event (OAE-2: ~94 Ma)

The rates of marine deoxygenation leading to Cretaceous Oceanic Anoxic Events are poorly recognized and constrained. If increases in primary productivity are the primary driver of these episodes, progressive oxygen loss from global waters should predate enhanced carbon burial in underlying sediments-the diagnostic Oceanic Anoxic Event relic. Thallium isotope analysis of organic-rich black shales from Demerara Rise across Oceanic Anoxic Event 2 reveals evidence of expanded sediment-water interface deoxygenation ~43 ± 11 thousand years before the globally recognized carbon cycle perturbation. This evidence for rapid oxygen loss leading to an extreme ancient climatic event has timely implications for the modern ocean, which is already experiencing large-scale deoxygenation.

Evidence for rapid weathering response to climatic warming during the Toarcian Oceanic Anoxic Event

Chemical weathering consumes atmospheric carbon dioxide through the breakdown of silicate minerals and is thought to stabilize Earth's long-term climate. However, the potential influence of silicate weathering on atmospheric pCO2 levels on geologically short timescales (103-105 years) remains poorly constrained. Here we focus on the record of a transient interval of severe climatic warming across the Toarcian Oceanic Anoxic Event or T-OAE from an open ocean sedimentary succession from western North America. Paired osmium isotope data and numerical modelling results suggest that weathering rates may have increased by 215% and potentially up to 530% compared to the pre-event baseline, which would have resulted in the sequestration of significant amounts of atmospheric CO2. This process would have also led to increased delivery of nutrients to the oceans and lakes stimulating bioproductivity and leading to the subsequent development of shallow-water anoxia, the hallmark of the T-OAE. This enhanced bioproductivity and anoxia would have resulted in elevated rates of organic matter burial that would have acted as an additional negative feedback on atmospheric pCO2 levels. Therefore, the enhanced weathering modulated by initially increased pCO2 levels would have operated as both a direct and indirect negative feedback to end the T-OAE.

Oceanic oxygenation events in the anoxic Ediacaran ocean

The ocean-atmosphere system is typically envisioned to have gone through a unidirectional oxygenation with significant oxygen increases in the earliest (ca. 635 Ma), middle (ca. 580 Ma), or late (ca. 560 Ma) Ediacaran Period. However, temporally discontinuous geochemical data and the patchy metazoan fossil record have been inadequate to chart the details of Ediacaran ocean oxygenation, raising fundamental debates about the timing of ocean oxygenation, its purported unidirectional rise, and its causal relationship, if any, with the evolution of early animal life. To better understand the Ediacaran ocean redox evolution, we have conducted a multi-proxy paleoredox study of a relatively continuous, deep-water section in South China that was paleogeographically connected with the open ocean. Iron speciation and pyrite morphology indicate locally euxinic (anoxic and sulfidic) environments throughout the Ediacaran in this section. In the same rocks, redox sensitive element enrichments and sulfur isotope data provide evidence for multiple oceanic oxygenation events (OOEs) in a predominantly anoxic global Ediacaran-early Cambrian ocean. This dynamic redox landscape contrasts with a recent view of a redox-static Ediacaran ocean without significant change in oxygen content. The duration of the Ediacaran OOEs may be comparable to those of the oceanic anoxic events (OAEs) in otherwise well-oxygenated Phanerozoic oceans. Anoxic events caused mass extinctions followed by fast recovery in biologically diversified Phanerozoic oceans. In contrast, oxygenation events in otherwise ecologically monotonous anoxic Ediacaran-early Cambrian oceans may have stimulated biotic innovations followed by prolonged evolutionary stasis.

Bacillus fermentation of soybeans

Kinema fermentations of Indian and Canadian No. 1 soybeans by Bacillus sp. DK-W1 and by mixed cultures of Bacillus sp. DK-W1 and Enterococcus faecium DK-C1 were essentially identical. The viable cell count of Bacillus increased from an initial 10(5) to 10(10) c.f.u./g wet wt after 48 h incubation at 37°C. The pH of the fermentation dropped from an initial 6.9 to about 6.4 after 8 h and then rose to 8.6 after 32 h, with a coincident increase in proteolytic activity and ammonia concentration. The fermentations containing E. faecium and Bacillus exhibited a greater initial pH decline and a slightly retarded subseqent increase in pH compared with fermentations with Bacillus only. The presence of E. faecium had no detectable effects on growth of the Bacillus, proteolytic activity, ammonia production or the final pH of the fermentations.

Sources of microorganisms in pozol, a traditional Mexican fermented maize dough

Freshly prepared pozol, a traditional Mexican fermented maize dough, contained (c.f.u./g wet wt): lactic acid bacteria, 10(4) to 10(6); aerobic mesophiles, 10(4) to 10(5); Enterobacteriaceae, 10(2) to 10(3); yeasts, 10(2) to 10(4); and mould propagules, <10(3). After 30 h at 28°C the numbers were, respectively: 10(9), 7×10(6), 5×10(5), 10(6) and 10(4). Soaking alkali-treated grains overnight allowed lactic acid bacteria, aerobic mesophiles and Enterobacteriaceae to grow and these then constituted the primary microbial flora of the pozol dough. Grinding in a commercial mill inoculated the dough with lactic acid bacteria, aerobic mesophiles, Enterobacteriaceae and yeasts. Other processing stages, including the nature of the surface upon which the balls were made, handling of the dough, and air, contributed only minor numbers of microbes compared with the two major sources, soaking and grinding. The pH of pozol fell from an initial value of 7.3 to 4.6 after 30 h incubation at 28°C. The numbers of Enterobacteriaceae and other aerobic mesophilic bacteria remained constant between 11 and 30 h incubation and there was no evidence of the acidic conditions having any lethal effects on these organisms.

Microbiology of pozol, a Mexican fermented maize dough

Mexican fermented maize dough, pozol, including traditional banana leaf-wrapped samples and material in plastic bags, was purchased. All samples were pH 4.7 to 5.7 approx. 12 h after preparation, pH declining to 3.6 to 3.9 after 6 to 9 days storage at ambient temperature. These latter samples had dry matter contents of 31% to 48% (w/w), 0.35% to 0.75% titratable acidity as lactic acid and lactic acid bacteria as predominant microbial flora at about 10(8) c.f.u./ml. The lactic acid bacteria included strains of Leuconostoc mesenteroides, Lactobacillus plantarum, Lactobacillus confusus, Lactococcus lactis and Lactococcus raffinolactis. Fungi were not found in the samples stored in plastic bags. The samples wrapped in banana leaf, however, developed a large surface mycoflora within 2 days. This included Geotrichum candidum, yeasts and moulds. The majority of the lactic acid bacteria and approx. 50% of yeasts hydrolysed starch to some extent. No Geotrichum isolate hydrolysed starch. Lactate was assimilated by all the Geotrichum isolates and by 17 of 39 yeast strains.

Sulfur record of rising and falling marine oxygen and sulfate levels during the Lomagundi event

Carbonates from approximately 2.3-2.1 billion years ago show markedly positive δ(13)C values commonly reaching and sometimes exceeding +10‰. Traditional interpretation of these positive δ(13)C values favors greatly enhanced organic carbon burial on a global scale, although other researchers have invoked widespread methanogenesis within the sediments. To resolve between these competing models and, more generally, among the mechanisms behind Earth's most dramatic carbon isotope event, we obtained coupled stable isotope data for carbonate carbon and carbonate-associated sulfate (CAS). CAS from the Lomagundi interval shows a narrow range of δ(34)S values and concentrations much like those of Phanerozoic and modern marine carbonate rocks. The δ(34)S values are a close match to those of coeval sulfate evaporites and likely reflect seawater composition. These observations are inconsistent with the idea of diagenetic carbonate formation in the methanic zone. Toward the end of the carbon isotope excursion there is an increase in the δ(34)S values of CAS. We propose that these trends in C and S isotope values track the isotopic evolution of seawater sulfate and reflect an increase in pyrite burial and a crash in the marine sulfate reservoir during ocean deoxygenation in the waning stages of the positive carbon isotope excursion.

Effects of temperature, pH, water activity and CO2 concentration on growth of Rhizopus oligosporus NRRL 2710

AIMS

To investigate the effects of temperature, pH, water activity (aw) and CO2 concentration on the growth of Rhizopus oligosporus NRRL 2710.

METHODS AND RESULTS

Hyphal extension rates from mycelial and spore inocula were measured on media with different aw (approximately 1.0, 0.98 and 0.96) and pH (3.5, 5.5 and 7.5) incubated at 30, 37 or 42 degrees C in atmospheres containing 0.03, 12.5 or 25% (v/v) CO2. The effects of environmental conditions on hyphal extension rate were modelled using surface response methodology. The rate of hyphal extension was very sensitive to pH, exhibiting a pronounced optimum at pH 5.5-5.8. The hyphal extension rate was less sensitive to temperature, aw or CO2, exhibiting maximum rates at 42 degrees C, a(w) approximately 1.0 and 0.03% (v/v) CO2.

CONCLUSIONS

The fastest hyphal extension rate (1.7 mm h(-1)) was predicted to occur at 42 degrees C, pH 5.85, a(w) approximately 1.0 and 0.03% CO2.

SIGNIFICANCE AND IMPACT OF THE STUDY

The present work is the first to model the simultaneous effects of temperature, pH, aw and CO2 concentration on mould growth. The information relates to tempe fermentation and to possible control of the microflora in Tanzanian cassava heap fermentations.

Effect of ammonia on the growth of Bacillus species and some other bacteria

The tolerance of 26 Bacillus species isolated from alkaline fermented foods, five other bacilli and nine non spore-forming bacteria to alkaline pH and ammonia was determined. All grew at pH 7, 8 and 9 in the presence of 930 mmol l-1 NH4 + at pH 7.0, and in the presence of NH3 concentrations up to 5 mmol l-1 at pH 7.0 and 8.0. At higher NH3 concentrations, growth of some of the bacteria was inhibited and at 500 mmol l-1 only B. pasteurii and B. pumilus grew. Bacteria from alkaline food fermentations included strains relatively sensitive to NH3 (inhibited by 50 mmol l-1) and relatively tolerant strains (grew in the presence of 300 mmol l-1) and there was no evidence that they were more tolerant to NH3 than bacteria not associated with these fermentations.

Protein utilization during soybean tempe fermentation

The aim was to identify to what extent proteins were utilized during the fermentation of bacteria-free tempe prepared with acidified soybean cotyledons and Rhizopus oligosporus NRRL 2710 at 30 degrees C. Dry matter declined continuously during the fermentation to 980 g/(kg of initial dry cotyledons) at 28 h, 910 g at 46 h (when the tempe was judged mature), and 835 g at 72 h. The decrease in dry matter was due mainly to reduction in crude lipid, amounting to 65 g/(kg of initial dry cotyledons) at 46 h and 135 g/(kg of initial dry cotyledons) at 72 h and representing approximately 70% and 80%, respectively, of the total dry matter loss. Protein oxidation (estimated from ammonia production) was 5 g at 28 h,10 g at 46 h, and 20 g/(kg of initial dry cotyledons) at 72 h. The total amount of soy protein hydrolyzed, including that incorporated into mold biomass, was estimated to be 80 g/(kg of initial dry cotyledons) at 28 h incubation, 95 g at 46 h, and 100 g at 72 h. The hydrolyzed protein at 46 h represented 25% of the initial protein. Of this hydrolyzed protein, it is suggested that approximately 65% remained in the tempe as amino acids and peptides, 25% was assimilated into mold biomass, and 10% was oxidized.

Glucosamine content of tempe mould, Rhizopus oligosporus

The glucosamine content of Rhizopus oligosporus NRRL 2710 mycelium grown in different media was determined. In Sabouraud dextrose broth the glucosamine content ranged from 51 g (kg dry biomass)(-1) for mycelial pellets less than 5 mm diameter to 107 g kg(-1) for pellets 16-35 mm diameter. Mycelium grown on Sabouraud dextrose agar contained 111 g glucosamine (kg dry biomass)(-1) while that grown on soymilk agar, used to simulate growth on soybeans in tempe, contained 82 g kg(-1). The estimation of glucosamine was reproducible, with a mean coefficient of variation of 4% for mycelial pellets and 11% for mycelium from agar media. It is suggested that a conversion factor of 12 g dry biomass (g glucosamine)(-1) is applicable to determine fungal biomass in tempe fermentation.

Decoupling of DNA excision repair and RNA transcription in translocation breaksite regions of plasmacytoma-susceptible BALB/cAnPt mice

Preferential repair of pyrimidine dimers in rodent cells is thought to be directly coupled to the RNA transcription machinery. The most compelling evidence for this notion is the finding that excision repair occurs more rapidly in the template strand of DNA of transcribed genes than in the non-template strand. A thorough test of this coupling concept by careful comparison of the rate of repair to the rate of transcription of a gene and its regulatory region has not been reported. In the present study, we used nuclear run-on as a measure of transcription in the c-myc and Pvt1 genes in normal B-lymphoblasts from plasmacytoma-susceptible (BALB/cAnPt) and plasmacytoma-resistant (DBA/2N) strains of mice. Previous studies have shown that these loci, but not c-abl or Dhfr are repaired differently in mouse strains: poorly in BALB/cAnPt but efficiently in DBA/2N. The results presented here indicate that in DBA/2N cells, run-on transcription from both DNA strands can be readily detected in the regions of c-myc and Pvt1 that were efficiently repaired. Unexpectedly, however, in BALB/cAnPt lymphoblasts, transcription was equivalent to that of DBA/2N, despite a dramatic reduction in efficiency of excision repair. This finding indicates that, in BALB/cAnPt lymphoblasts, DNA repair 5' to c-myc and in Pvt1 is decoupled from the RNA transcription machinery. We postulate that this dissociation of repair and transcription represents a BALB/cAnPt-specific defect in a component of the transcription/repair complex that specifically compromises repair activity but not transcription. This defect may be responsible for the inability of normal BALB/cAnPt lymphoblasts to repair DNA sequences in the c-myc 5' flank and the Pvt1 gene, inducing gene-specific instability that predisposes these loci to genetic accidents, including chromosomal translocation, retroviral integration and other mutations.

Munkoyo beverage, a traditional Zambian fermented maize gruel using Rhynchosia root as amylase source

A typical munkoyo beverage was made by fermenting Rhynchosia heterophylla root extract-cooked maize meal mixture with Lactobacillus confusus LZI and Saccharomyces cerevisiae YZ20. The fermented munkoyo beverage had a pH of 3.3, lactic acid content of 60 mmol/l, ethanol 320-410 mmol/l and a characteristic 'munkoyo' aroma. L. confusus, used alone, produced a beverage with a faint munkoyo flavour note whilst beverage produced with S. cerevisiae alone seemed not to have a typical munkoyo note. R. heterophylla root extract converted 75% of the starch in sterile cooked maize meat to maltose (80% of total sugars), maltotriose (17%) and glucose (3%) in I h at 45 degrees C. During fermentation by the mixed culture or the yeast alone most of the maltose was utilised but little or none of the maltotriose. The ratio of yeast to lactic acid bacteria in the starter culture affected the rate of production of ethanol but had no effect on the growth or acid production by the bacterium. To obtain a munkoyo beverage with the desired low alcohol concentration (< 100 mmol/l), the ratio of yeast concentration (cfu/ml) to Lactobacillus concentration in the starter culture should be 1:1000 or less and the beverage should be fermented for 24 h only.

Control of ammonia formation during Bacillus subtilis fermentation of legumes

The control of ammonia formation during the Bacillus subtilis fermentation of autoclaved, roasted soybean cotyledons (Glycine max) and of autoclaved African locust bean cotyledons (Parkia spp.) was investigated. Addition of NaCl, 1.5 mol (kg wet cotyledons)-1, part way through the fermentation inhibited ammonia formation and softening of the cotyledons. Addition of glycerol, 1.7 mol (kg wet cotyledons)-1 part way through the fermentation inhibited alkalinisation and ammonia formation while allowing enzymic activity and softening of the cotyledons to continue. Restriction of the oxygen supply by incubating the cotyledons in a sealed container also prevented excessive ammonia production and increase in pH value. Fermentations conducted in sealed containers with an air to cotyledons ratio of approximately 130-175 ml air (g wet cotyledons)-1 supported good microbial growth and proteolysis without the formation of detectable ammonia aroma.

Sapal: a traditional fermented taro [Colocasia esculenta (L.) Schott] corm and coconut cream mixture from Papua New Guinea

Sapal is a traditional fermented food made by mixing cooked, grated taro [Colocasia esculenta (L.) Schott] corm with coconut cream and allowing it to ferment at ambient temperature. The fermentation was primarily due to heterofermentative lactic acid bacteria, which reached 10(10) cfu/ml. Seven out of 10 isolated bacterial strains were identified as Leuconostoc mesenteroides or Leuc. paramesenteroides. The initial microbial flora was derived from the coconut cream. Yeasts grew on the surface of the sapal in the later stages of the fermentation. Overnight storage of the grated taro corm resulted in the glucose concentration increasing from 1.1 to about 5 g/l. During the fermentation the glucose concentration decreased to undetectable levels. The pH value fell from an initial value of 6.1 to 4.1 after 24 h.

Retroviral enhancer insertion 5' of c-myc in two translocation-negative mouse plasmacytomas upregulates c-myc expression to different extents

Essentially all murine plasmacytomas have deregulated c-myc expression that is typically brought about by chromosomal translocations between the c-myc/Pvt-1 locus and one of the immunoglobulin loci. ABPC 22 and RFPC 2782 are BALB/c plasmacytomas that lack chromosomal translocations yet have Southern blot evidence of c-myc gene rearrangements. In this report we show that proviral integrations 5' of the c-myc gene can deregulate c-myc expression in mouse plasmacytomas. Analysis of DNA sequences 5' of the c-myc genes from both tumors demonstrated that rearrangements were caused by retroviral integrations 5' of c-myc exon 1. The proviral insertion in RFPC 2782 was associated with a high steady-state c-myc mRNA level comparable to that seen in plasmacytomas with typical translocations. An analogous proviral insertion in ABPC 22 was associated with a c-myc RNA level that was only 38% of that of RFPC 2782. Nuclear run-on studies of c-myc transcription showed that ABPC 22 has both a lower rate of transcription and a greater degree of transcriptional attenuation than RFPC 2782. DNA sequencing of the long terminal repeat of each tumor provirus showed that the ABPC 22 provirus harbors a deletion of one of the two direct repeats in the viral enhancer, whereas both repeats are present in the RFPC 2782 provirus. These data indicate that maximum LTR enhancer effectiveness in plasmacytomas in vivo requires the presence of both LTR direct repeats. The documentation of the low level of steady-state c-myc mRNA in ABPC 22 supports the notion that deregulated c-myc expression, even at low steady state levels, is effective in supporting the development of plasmacytomas.

Causes of conductance change in yeast cultures

The conductance change due to growth of Saccharomyces cerevisiae Y112, Zygosaccharomyces bailii M and Rhodotorula rubra NCYC 63 in culture media containing glucose, tartrate pH buffer and ammonium ions as sole nitrogen source was compared with that in a medium containing L-asparagine as sole nitrogen source. Decreases in conductance were observed in glucose-ammonium cultures of all three yeasts while little change occurred in cultures with L-asparagine as sole nitrogen source. This supports the hypothesis that the metabolic activity primarily responsible for conductance change in yeast cultures is the uptake of charged ammonium ions as nitrogen source and the reaction of protons with pH buffer compounds. Rhodotorula rubra cultures with L-asparagine as sole carbon source caused large increases in conductance with growth. Chemical analyses of culture filtrates showed that this increase in conductance was due to use of L-asparagine as carbon source and the excretion of nitrogen surplus to biosynthetic needs as ammonium. In addition, the production of aspartate, acetate and bicarbonate contributed to the increase in conductance.

Nonhomologous recombination at sites within the mouse JH-C delta locus accompanies C mu deletion and switch to immunoglobulin D secretion

Plasma cells secrete immunoglobulins other than immunoglobulin M (IgM) after a deletion and recombination in which a portion of the immunoglobulin heavy-chain locus (IgH), from the 5'-flanking region of the mu constant-region gene (C mu) to the 5'-flanking region of the secreted heavy-chain constant-region gene (CH), is deleted. The recombination step is believed to be targeted via switch regions, stretches of repetitive DNA which lie in the 5' flank of all CH genes except delta. Although serum levels of IgD are very low, particularly in the mouse, IgD-secreting plasmacytomas of BALB/c and C57BL/6 mice are known. In an earlier study of two BALB/c IgD-secreting hybridomas, we reported that both had deleted the C mu gene, and we concluded that this deletion was common in the normal generation of IgD-secreting cells. To learn how such switch recombinations occur in the absence of a switch region upstream of the C delta 1 exon, we isolated seven more BALB/c and two C57BL/6 IgD-secreting hybridomas. We determined the DNA sequences of the switch recombination junctions in eight of these hybridomas as well as that of the C57BL/6 hybridoma B1-8. delta 1 and of the BALB/c, IgD-secreting plasmacytoma TEPC 1033. All of the lines had deleted the C mu gene, and three had deleted the C delta 1 exon in the switch recombination event. The delta switch recombination junction sequences were similar to those of published productive switch recombinations occurring 5' to other heavy-chain genes, suggesting that nonhomologous, illegitimate recombination is utilized whenever the heavy-chain switch region is involved in recombination.

The in vivo generation of murine IgD-secreting cells is accompanied by deletion of the C mu gene and occasional deletion of the gene for the C delta 1 domain

Mature, resting rodent, and primate B lymphocytes express two membrane Ig isotypes, IgM and IgD. Although membrane IgD production by these cells is regulated at a transcriptional level, and does not require deletion of the C mu gene, C mu has been deleted in all of the IgD-secreting tumor cells that have been studied. These IgD-secreting tumors, which include two mineral oil-induced plasmacytomas and three IgD-switch variants of an IgM-secreting hybridoma, might not, however, be representative of the rare IgD-secreting cells generated in response to an immune stimulus. A recent study of mice injected with a goat antibody to mouse IgD has demonstrated the generation of a relatively large secretory IgD response in these animals. We have now produced hybridomas by fusing spleen cells from these mice with a non-Ig-secreting plasmacytoma. Two of these hybridomas, KWD-1 and KWD-2, secrete IgD and express cell membrane IgD. Both of these hybridomas were found to have deleted the C mu gene. KWD-2 produces a delta-chain mRNA and a delta-chain protein similar in size to those previously reported for normal secreted mouse IgD; however, KWD-1 synthesizes a secretory delta-chain mRNA that is approximately 0.25 kb smaller than the KWD-2 secretory delta-chain mRNA and secretes IgD with a delta-chain that is approximately 21 kDa smaller than the secretory delta-chain of KWD-2. ELISA studies with epitope-defined anti-delta mAb indicate that KWD-2 has both delta Fc (C delta 3) [corrected] and delta Fd (C delta 1) [corrected] determinants, whereas KWD-1 has delta Fc but not delta Fd. These studies also demonstrate that the Ag-binding site of KWD-1 is not deleted because KWD-1 specifically binds goat IgG. Northern blot analyses with exon-specific probes indicate that while both KWD-1 and KWD-2 synthesize kappa-chain mRNA and delta-chain mRNA that includes the VH, C delta hinge, and C delta 3 exons, the C delta 1 exon is present only on the KWD-2 delta-chain mRNA. Southern blot analysis confirms that the C delta 1 exon has been deleted in KWD-1, but not KWD-2. We have previously noted that a secretory delta-chain mRNA that is similar in size to that produced by KWD-1 accounts for approximately 25% of the splenic secretory delta-chain mRNA produced by goat anti-mouse IgD antibody-injected mice.(ABSTRACT TRUNCATED AT 400 WORDS)

The in vivo generation of murine IgD-secreting cells is accompanied by deletion of the C mu gene and occasional deletion of the gene for the C delta 1 domain

Mature, resting rodent, and primate B lymphocytes express two membrane Ig isotypes, IgM and IgD. Although membrane IgD production by these cells is regulated at a transcriptional level, and does not require deletion of the C mu gene, C mu has been deleted in all of the IgD-secreting tumor cells that have been studied. These IgD-secreting tumors, which include two mineral oil-induced plasmacytomas and three IgD-switch variants of an IgM-secreting hybridoma, might not, however, be representative of the rare IgD-secreting cells generated in response to an immune stimulus. A recent study of mice injected with a goat antibody to mouse IgD has demonstrated the generation of a relatively large secretory IgD response in these animals. We have now produced hybridomas by fusing spleen cells from these mice with a non-Ig-secreting plasmacytoma. Two of these hybridomas, KWD-1 and KWD-2, secrete IgD and express cell membrane IgD. Both of these hybridomas were found to have deleted the C mu gene. KWD-2 produces a delta-chain mRNA and a delta-chain protein similar in size to those previously reported for normal secreted mouse IgD; however, KWD-1 synthesizes a secretory delta-chain mRNA that is approximately 0.25 kb smaller than the KWD-2 secretory delta-chain mRNA and secretes IgD with a delta-chain that is approximately 21 kDa smaller than the secretory delta-chain of KWD-2. ELISA studies with epitope-defined anti-delta mAb indicate that KWD-2 has both delta Fc (C delta 3) [corrected] and delta Fd (C delta 1) [corrected] determinants, whereas KWD-1 has delta Fc but not delta Fd. These studies also demonstrate that the Ag-binding site of KWD-1 is not deleted because KWD-1 specifically binds goat IgG. Northern blot analyses with exon-specific probes indicate that while both KWD-1 and KWD-2 synthesize kappa-chain mRNA and delta-chain mRNA that includes the VH, C delta hinge, and C delta 3 exons, the C delta 1 exon is present only on the KWD-2 delta-chain mRNA. Southern blot analysis confirms that the C delta 1 exon has been deleted in KWD-1, but not KWD-2. We have previously noted that a secretory delta-chain mRNA that is similar in size to that produced by KWD-1 accounts for approximately 25% of the splenic secretory delta-chain mRNA produced by goat anti-mouse IgD antibody-injected mice.(ABSTRACT TRUNCATED AT 400 WORDS)

Alternative splicing of RNAs transcribed from the human c-myb gene

An alternative splicing event in which a portion of the intron bounded by the vE6 and vE7 exons with v-myb homology is included as an additional 363-nucleotide coding exon (termed E6A or coding exon 9A) has been described for normal and tumor murine cells that express myb. We show here that this alternative splicing event is conserved in human c-myb transcripts. In addition, another novel exon (termed E7A or coding exon 10A) is identified in human c-myb mRNAs expressed in normal and tumor cells. Although the myb protein isoform encoded by murine E6A-containing mRNA is larger than the major c-myb protein, the predicted products of both forms of human alternatively spliced myb transcripts are 3'-truncated myb proteins that terminate in the alternative exons. These proteins are predicted to lack the same carboxy-terminal domains as the viral myb proteins encoded by avian myeloblastosis virus and E26 virus. The junction sequences that flank these exons closely resemble the consensus splice donor and splice acceptor sequences, yet the alternative transcripts are less abundant than is the major form of c-myb transcripts. The contribution that alternative splicing events in c-myb expression may make on c-myb function remains to be elucidated.

Altered myc gene transcription and intron-induced stabilization of myc RNAs in two mouse plasmacytomas

Accumulation of unusually high amounts of larger-than-normal c-myc mRNAs occurs in two mouse plasmacytomas, TEPC 1165 and TEPC 2027. Southern blot and DNA sequence analyses showed that both tumors have undergone translocations of immunoglobulin heavy chain loci to positions 5' of the c-myc gene promotors resulting in removal of DNA sequences encoding a negative transcriptional regulatory element. In contrast to other mouse plasmacytomas, TEPC 1165 and TEPC 2027 rearranged myc genes show increased transcription, partially explaining their abundance of myc RNA. Similar to other mouse plasmacytomas, the abundance of myc RNA in TEPC 1165 and TEPC 2027 is also influenced by increased stability of structurally atypical myc RNAs. Two myc mRNAs are found in TEPC 2027, a 2.4 kb species including all 3 myc exons and a 4.0 kb species with the 3 exons plus the first intron. The two major myc mRNAs in TEPC 1165, 3.0 and 3.9 kb species, also include all three myc exons plus portions of the first intron. S1 nuclease protection analyses show that the 5' initiation and 3' untranslated (UT) regions of the unusual TEPC 1165 RNAs are normal showing that the size differences arise solely from inclusion of first intron sequences in the large myc RNAs. DNA sequence analysis showed that the presence of first intron sequences in the large myc RNAs is due to mutations affecting the splice donor region at the 3' end of exon 1 in both tumors. SDS-PAGE analysis of immunoprecipitated TEPC 1165 and TEPC 2027 myc proteins showed them to be of normal electrophoretic mobility but no more abundant than in a pre-B cell line 18-81 that contains at least 10 fold less myc RNA. The 4.0 kb myc mRNA of TEPC 2027 is atypically stable while the 2.4 kb myc mRNA undergoes normal rapid turnover within the same cell, demonstrating that the presence of first intron sequences in the large myc RNA stabilizes it despite the presence of 3' UT and putative exon 1 destabilizing sequences. These results show that myc intron 1 sequences can counteract the effect of 3' UT region destabilizing sequences in myc RNA and suggest that the increased myc RNA stability noted in TEPC 1165 and TEPC 2027 is largely due to the presence of the intron 1 sequences.(ABSTRACT TRUNCATED AT 400 WORDS)

Amino acids at the site of V kappa-J kappa recombination not encoded by germline sequences

Murine V kappa-J kappa recombination is characterized by a maintenance of size at the site of recombination and the use of nucleic acids found only in germline sequences. This is in contrast to heavy chain VH-D-JH assembly where random nucleotides are added at the recombination sites to produce considerable size variation, even though the heptamer/nonomer recombination sequences are identical in both kappa and heavy chain genes. We have examined the origin of an unusual amino acid, Ile, found at the site of V kappa-J kappa recombination in antigalactan antibodies, by sequence analysis of the corresponding rearranged and germline genes. Results indicate that the Ile codon can be generated by use of a single nucleotide 3' of the V kappa segment in combination with the second and third nucleotides of the first codon of J kappa 5 or J kappa 4. However, several antigalactan antibodies express Ile in combination with J kappa 2. An Ile codon cannot be generated by recombination in any reading frame between germline V kappa and J kappa 2 segments. These results suggest that the origin of the Ile codon in lines using J kappa 2 may represent a novel even in murine light chain assembly, possibly similar to the de novo addition of nucleotides observed in heavy chain gene recombination.

Selection of pH buffers for use in conductimetric microbiological assays

Many metabolic activities of micro-organisms lead to changes in the pH value of cultures and consequently pH buffer compounds are potentially a major source of conductivity changes in cultures. To maximize changes in conductivity associated with microbial growth the pH buffer-associated changes should occur in a direction that reinforces those due to other metabolic activities. In agreement with this, studies with Escherichia coli showed that fermentation of glucose and aerobic growth on L-alanine yielded greater changes in the conductivity of media containing Tris(hydroxymethyl)aminomethane or L-histidine buffers than in a medium containing phosphate buffer, whereas aerobic growth on glucose or succinate yielded greater changes with phosphate buffer than with Tris(hydroxymethyl)aminomethane or L-histidine buffers. Criteria for the selection of appropriate pH buffer compounds are presented.

Prevention of autoimmune uveitis by competitive immunization with bovine gamma globulin

The effect of antigenic competition on the development of autoallergic experimental uveitis and autoallergy to ocular antigens was studied. Strain 13 guinea pigs were immunized with adjuvants containing either National Institutes of Health strain retina-uvea extract or retina-uvea extract plus bovine gamma globulin (BGG). They were later reimmunized with ocular extract and BGG or ocular extract alone, in adjuvant. They were observed weekly by slit-lamp examination. At the end of the study, they were skin tested using strain 13 retina-uvea extract. The eyes of certain groups were examined histologically. Immunization and reimmunization with ocular extract produced uveitis. The addition of BGG to the initial immunization prevented the development of uveitis even after reimmunization with ocular extract alone. It did not, however, necessarily prevent the development of delayed type skin sensitivity to retina-uveal extract.

Sources of conductance changes during bacterial reduction of trimethylamine oxide to trimethylammonium in phosphate buffer

The sources of conductance changes during reduction of trimethylamine oxide to trimethylamine by Escherichia coli with formate as electron donor and in the presence of phosphate buffer were investigated. Theoretical considerations and experimental results suggest that the major source of conductance change is the conversion of dihydrogen phosphate to hydrogen phosphate. This transformation contributes almost twice as much to the total conductance change as does the conversion of uncharged trimethylamine oxide to charged trimethylammonium.

Mouse IgD half molecules with shortened IgD heavy chain result from alterations within C delta locus

An unusually small (51 KD) IgD myeloma protein was isolated from secretions of TEPC 1017 generation (gen) 24. The delta-chain mRNA and the delta-chain gene in this tumor were compared with those of TEPC 1017 of earlier generations. The gen 24 protein contained one normal-sized kappa-type light chain (21 KD) and one unusually short delta-heavy chain (30 KD). The delta-heavy chain was 15 KD shorter than that of TEPC 1017 of earlier generations, owing to a delta-mRNA (1.15 kb) which was 600 bp shorter than that of TEPC 1017 of earlier generations. TEPC 1017 is a tetraploid tumor, and the gen 24 appears to contain at least two different deletions on different chromosomes. The short mRNA was produced from one of these altered delta-chain genes which had a productive VDJ rearrangement but which had lost the C delta 3 domain and perhaps the C delta H domain as well. Despite these genetic insults, RNA splicing produced delta-mRNA with secreted termini and mRNA with membrane-binding termini. It is suggested that the mouse C delta gene has an unusual predilection for deletions because it normally lacks any vestige of C delta 2 and, during i.p. passage, it suffered further deletions or alterations.

Mouse IgD half molecules with shortened IgD heavy chain result from alterations within C delta locus

An unusually small (51 KD) IgD myeloma protein was isolated from secretions of TEPC 1017 generation (gen) 24. The delta-chain mRNA and the delta-chain gene in this tumor were compared with those of TEPC 1017 of earlier generations. The gen 24 protein contained one normal-sized kappa-type light chain (21 KD) and one unusually short delta-heavy chain (30 KD). The delta-heavy chain was 15 KD shorter than that of TEPC 1017 of earlier generations, owing to a delta-mRNA (1.15 kb) which was 600 bp shorter than that of TEPC 1017 of earlier generations. TEPC 1017 is a tetraploid tumor, and the gen 24 appears to contain at least two different deletions on different chromosomes. The short mRNA was produced from one of these altered delta-chain genes which had a productive VDJ rearrangement but which had lost the C delta 3 domain and perhaps the C delta H domain as well. Despite these genetic insults, RNA splicing produced delta-mRNA with secreted termini and mRNA with membrane-binding termini. It is suggested that the mouse C delta gene has an unusual predilection for deletions because it normally lacks any vestige of C delta 2 and, during i.p. passage, it suffered further deletions or alterations.

Mouse immunoglobulin D: construction and characterization of a cloned delta chain cDNA

TEPC 1017 is a BALB/c plasmacytoma that synthesizes IgD in large enough amounts to permit the isolation of mRNA for mouse delta chains. cDNA has been prepared from this mRNA, and an 880-base-pair fragment of it has been cloned by recombinant DNA techniques. The hybridization selection technique has been used to show that this cDNA clone specifically binds only mRNA that can be translated into immunoprecipitable delta chains. the sequence of a portion of this clone has been determined and, when translated, shows homology with the C delta 3 of a human myeloma protein. Using this cDNA clone as a probe, we have found that several different-sized delta RNAs are present in TEPC 1017 and in another IgD-secreting plasmacytoma, TEPC 1033.

The induction of immunologic tolerance with type III pneumococcal polysaccharide cross-linked or coupled to protein

Type III pneumococcal polysaccharide molecules were linked to one another, i. e. cross-linked. The product was essentially insoluble in saline. Large pieces weighing 1-2 mg were inserted into mice. They produced immunologic paralysis or immune tolerance. When placed intraperitoneally in millipore chambers the cross-linked polysaccharide did not have any apparent effect, for the mice were not tolerized. When pneumococcal polysaccharide was linked to a protein, the amount of polysaccharide required to cause tolerance or immunity was essentially the same as the amount of free pure soluble polysaccharide. In addition, Xenopus laevis eggs were injected with a different antigen, bovine gamma globulin, and then with antibody to that antigen. Twelve of the twelve eggs so injected changed shape. Equal numbers of other eggs injected twice with the antigen or twice with the antibody did not change shape.

Hapten-specific delayed hypersensitivity to epsilon-2,4-dinitrophenyl-L-lysine-Ficoll in guinea pigs immunized with 2,4-dinitrophenyl-keyhole limpet hemocyanin

After active immunization with 2,4-dinitrophenyl-keyhole limpet hemocyanin (DNP-KLH), 2,4-dinitropheynl-L-lysine (DNPL)-Ficoll may elicit indurated, erythematous skin reactions lasting 24-72 h. Histological sections of these reactions, examined by microscope techniques, showed they contained polymorphonuclear leukocytes and perivascularly situated lymphocytes and macrophages, but had very few basophils. Consequently, the reaction was interpreted as having an immediate component and a component typical of delayed hypersensitivity; this indicated that the delayed reaction could be specific for the DNP hapten. Although this delayed type of skin reaction was not transferred to recipients with anti-DNP-KLH serum, one pool of that serum did sensitize guinea pigs so that they could respond with a different skin reaction after challenge with DNPL-Ficoll. This reaction was soft, pale pink, and lasted for 24 h. Histologically, it contained only a few polymorphonuclear leukocytes. It differed from the delayed reaction in actively immunized animals in that it lacked induration, and was devoid of lymphocytes and macrophages.

Hapten-specific leukocyte migration inhibition. I. Inhibition of cells from animals immunized with DNP-KLH by epsilon-DNP-L-lysine Ficoll

Guiena pigs were immunized with dinitrophenyl-keyhole limpet hemocyanin (DNP-KLH) or with hemocyanin in complete Freud's adjevant. The migration of oil-induced peritoneal exudate cells was measured in the presence and absence of epsilon-dinitrophenyl-lysine-tyrosinyl Ficoll (DNPL-F). When the cells came from animals immunized with DNP-KLH their migration was inhibited by DNPL-F. Control cells from animals immunized with KLH or not immunized migrated normally in the presence of DNPL-F.

An analysis of the substrate-induced rate effect in the phosphoglucomutase system

The rate constant for the catalytic transfer of the active-site PO3 group from rabbit muscle phosphoglucomutase to the hydroxyl group of a water molecule is about 3 x 10(-8) s-1 under optimal reaction conditions, but in the absence of the normal substrate, viz., at pH 7.5 and 30 degrees C, in the presence of saturating Mg2+; the corresponding constant for transfer to the 6-hydroxyl group of glucose 1-phosphate under analogous conditions, about 1000 s-1, is larger than this by some 3 x 10(10)-fold. Since no single factor appears to be capable of providing a rationale for a majority of this "substrate-induced rate effect" (Ray, jr., W.J., and Long, J.W. (1976), Biochemistry, the preceding paper in this issue), the change in the PO3-transfer rate produced by binding various parts of the phosphoglucosyl moiety to the enzyme, both separately and concurrently, was investigated. The rate of PO3 transfer to water is increased by up to 1000-fold by binding entities that provide the active site with a second PO3 group, e.g., ethyl phosphate or inorganic phosphite. Using an alcoholic acceptor further increases transfer efficiency (in the presence of bound phosphite): increase with methanol, about 2000-fold on a molar basis. The reactivities of ten other primary aliphatic alcohols vary by nearly 600-fold as the acidity of the PO3 acceptor is varied over a 4000-fold range. Although no straightforward relationship is observed between the efficiency of an alcohol as an acceptor and its acidity - presumably because of complications due to steric effects, for example - an increased transfer rate of 100-fold, relative to the water reaction, is estimated for a simple primary alcohol with a pKa similar to that expected for the 6-hydroxyl group of glucose 1-phosphate, when the alcohol is present at a concentration of 1 M. Joining an alcoholic acceptor and a PO3 group via five apparently inert bridging units changes PO3 transfer to an intramolecular process; in the case of 1,4-butanediol monophosphate the rate of transfer also increases by 240-fold, relative to the analogous reaction in the presence of 1 M propanol and bound inorganic phosphite. Comparable values also are obtained in comparisons of PO3 transfer rates for trans- 1,4-butenediol and 1,4-butynediol monophosphates relative to 1 M allyl and propargyl alcohols, respectively, in the presence of bound phosphite. An increased rate of transfer also is produced by binding the xylosyl part of the glucose ring, either when the acceptor is an hydroxyl group attached to the ring or when it is the hydroxyl group of a water molecule, e.g., as in the water reaction facilitated by bound xylose 1-phosphate. These and other results suggest that most of the differences between the rates of the water reaction and the glucose 1-phosphate reaction can be rationalized in terms of four fairly discrete factors whose approximate values are as follows: the PO4 factor, 1000-fold; the C-OH/H-OH factor, 100-fold; the nucleophile-binding factor, 250-fold; and the (CHOH)3-bridging factor, 200-fold...

Prevention of experimental allergic uveitis. Treatment and methotrexate

These experiments were undertaken to determine if methotrexate therapy, initiated after immunization, could prevent the development of experimental allergic uveitis. Strain 13 guinea pigs were immunized with Strain 13 guinea pig retina-uvea extract that had been emulsified in Freund complete adjuvant. Some were treated with methotrexate twice a week until the 21st day. Each week, all of their eyes were examined with a slit-lamp. At the end of the study, some were skin tested, and the sera of selected animals were tested by immunodiffusion for antibody. The eyes of certain groups were examined histologically. Results show methotrexate prevented the development of this type of uveitis, even when therapy was initiated seven days after immunization. The disease did not appear after therapy was stopped. Methotrexate also inhibited the development of skin sensitivity and antibody to retina-uvea antigen.

DNP-Lys-ficoll: a T-independent antigen which elicits both IgM and IgG anti-DNP antibody-secreting cells

The 2,4-dinitrophenyl-lysyl derivative of Ficoll (DNP-Lys-Ficoll) was prepared and examined for immunogenicity. This antigen elicited large numbers of DNP-specific plaque-forming cells (PFC) of the IgM and IgG2 class in the spleens of C57BL/6 mice. Similar responses were observed in congenitally athymic (nu/nu) mice and in their littermates indicating that DNP-Lys-Ficoll is a T-independent antigen. The responses of nu/nu mice included a large number of IgG2 DNP-specific PFC, indicating that IgG responses can be initiated in the absence of mature thymus-dependent (T) lymphocytes. Cell transfer studies confirmed the T independence of the response and indicated that priming with DNP-Lys-Ficoll induces only a very meager degree of memory. Because they can be obtained in large quantities and in relatively pure form, DNP-Lys-Ficoll and other hapten conjugates of Ficoll should prove most valuable in the delineation of the mode of activation of precursors of antibody-secreting cells by T-independent antigens.