Seawater barium and sulfide removal improved marine habitability for the Cambrian Explosion of early animals.

An increase in atmospheric pO2 has been proposed as a trigger for the Cambrian Explosion at ∼539-514 Ma but the mechanistic linkage remains unclear. To gain insights into marine habitability for the Cambrian Explosion, we analysed excess Ba contents (Baexcess) and isotope compositions (δ138Baexcess) of ∼521-Myr-old metalliferous black shales in South China. The δ138Baexcess values vary within a large range and show a negative logarithmic correlation with Baexcess, suggesting a major (>99%) drawdown of oceanic Ba inventory via barite precipitation. Spatial variations in Baexcess and δ138Baexcess indicate that Ba removal was driven by sulfate availability that was ultimately derived from the upwelling of deep seawaters. Global oceanic oxygenation across the Ediacaran-Cambrian transition may have increased the sulfate reservoir via oxidation of sulfide and concurrently decreased the Ba reservoir by barite precipitation. The removal of both H2S and Ba that are deleterious to animals could have improved marine habitability for early animals.

Atmospheric oxygenation as a potential trigger for climate cooling.

Secular changes in atmospheric CO2 and consequent global climate variations, are commonly attributed to global outgassing and the efficiency of silicate weathering, which may have been linked to mountain formation, land/arc distribution, and plant colonization through geological time. Although oxidative weathering has been shown to exert a significant role in the propagation of weathering fronts through the oxidation of Fe-bearing minerals, the influence of atmospheric O2 concentration (pO2) on silicate weathering, CO2 consumption, and global climate has not been thoroughly evaluated. This study presents a numerical model aimed at estimating the effects of pO2 on the climate, considering the influence of pO2 on the regolith thickness and thus weathering duration of granitic domains. Our model simulations reveal that an increase in weathering efficiency, through deeper penetration of the oxidative weathering front in the granitic regolith, would independently introduce a steady-state climate cooling of up to ∼8 °C, in step with one-order of magnitude rise in pO2. This temperature change may have repeatedly initiated the runaway ice-albedo feedback, leading to global glacial events (e.g., Neoproterozoic Snowball Earth). Increasing granitic weathering efficiency caused by a substantial pO2 increase may also have contributed to the development of icehouse climate during the Phanerozoic.

Lithium isotopic constraints on the evolution of continental clay mineral factory and marine oxygenation in the earliest Paleozoic Era.

The evolution of oxygen cycles on Earth's surface has been regulated by the balance between molecular oxygen production and consumption. The Neoproterozoic-Paleozoic transition likely marks the second rise in atmospheric and oceanic oxygen levels, widely attributed to enhanced burial of organic carbon. However, it remains disputed how marine organic carbon production and burial respond to global environmental changes and whether these feedbacks trigger global oxygenation during this interval. Here, we report a large lithium isotopic and elemental dataset from marine mudstones spanning the upper Neoproterozoic to middle Cambrian [~660 million years ago (Ma) to 500 Ma]. These data indicate a dramatic increase in continental clay formation after ~525 Ma, likely linked to secular changes in global climate and compositions of the continental crust. Using a global biogeochemical model, we suggest that intensified continental weathering and clay delivery to the oceans could have notably increased the burial efficiency of organic carbon and facilitated greater oxygen accumulation in the earliest Paleozoic oceans.

Revisiting marine redox conditions during the Ediacaran Shuram carbon isotope excursion.

The Neoproterozoic carbonate record contains multiple carbon isotope anomalies, which are the subject of intense debate. The largest of these anomalies, the Shuram excursion (SE), occurred in the mid-Ediacaran (~574-567 Ma). Accurately reconstructing marine redox landscape is a clear path toward making sense of the mechanism that drives this δ13 C anomaly. Here, we report new uranium isotopic data from the shallow-marine carbonates of the Wonoka Formation, Flinders Ranges, South Australia, where the SE is well preserved. Our data indicate that the δ238 U trend during the SE is highly reproducible across globally disparate sections from different depositional settings. Previously, it was proposed that the positive shift of δ238 U values during the SE suggests an extensive, near-modern level of marine oxygenation. However, recent publications suggest that the fractionation of uranium isotopes in ferruginous and anoxic conditions is comparable, opening up the possibility of non-unique interpretations of the carbonate uranium isotopic record. Here, we build on this idea by investigating the SE in conjunction with additional geochemical proxies. Using a revised uranium isotope mass balance model and an inverse stochastic carbon cycle model, we reevaluate models for δ13 C and δ238 U trends during the SE. We suggest that global seawater δ238 U values during the SE could be explained by an expansion of ferruginous conditions and do not require a near-modern level of oxygenation during the mid-Ediacaran.

Cryptotanshinone alleviates chemotherapy-induced colitis in mice with colon cancer via regulating fecal-bacteria-related lipid metabolism.

Patients with colorectal cancer treated with 5-fluorouracil (5-FU) and irinotecan (CPT-11) exhibit a risk for chemotherapy-induced colitis (CIC) that may lead to fatal consequences. Cryptotanshinone (CTS) is a natural compound extracted from the root of Salvia miltiorrhiza Bunge that shows potent antitumor activities. We previously reported CTS relieved 5-FU/ CPT-11 induced colitis in tumor-free mice. In this study, we studied the effect of CTS on 5-FU/ CPT-11 induced colitis in mice with colitis associated colon cancer (CAC). The effects of CTS on CIC were evaluated by disease activity index (DAI) and histological assessment via hematoxylin-and-eosin staining. Serum lipids and lipid-metabolic enzymes were detected by commercial kits. Fecal microbial diversity was detected by 16S ribosomal RNA gene sequencing. To find the role of fecal bacteria in CAC mice with 5-FU/ CPT-11 induced colitis, pseudo-germ-free mice were established by intragastric administration of mixed antibiotics. Except for decreasing tumor number (3 ± 1 vs 6 ± 1, p < 0.05), CTS significantly alleviated DAI (1.9 ± 0.6 vs 2.6 ± 0.5, p < 0.05) and regulated serum lipids in CAC mice with 5-FU/ CPT-11induced colitis. Compared with model group, CTS significantly increased serum triglycerides (TG) (1.13 ± 0.26 mM vs 0.79 ± 0.03 mM, p < 0.05), high density lipoprotein (HDL) (3.88 ± 0.1 mM vs 3.28 ± 0.05 mM, p < 0.001) and oxidized low-density lipoprotein (oxLDL) (288.12 ± 65.92 ng/mL vs 150.72 ± 42.13 ng/mL, p < 0.05) level but decreased serum adiponectin level (1177.47 ± 179.2 pg/mL vs 1523.43 ± 91.8 pg/mL, p < 0.05). Among fecal bacteria significantly correlated with lipid metabolism, CTS significantly decreased the abundance of g__norank_f__Muribaculaceae (21.15 % ± 5.7 % vs 41.84 ± 12.0 %, p < 0.01) but increased that of g_Lactobacillus (11.13 % ± 6.6 % vs 5.7 % ± 4.6 %, p < 0.05), g__Alistipes (3.66 % ± 0.7 % vs 1.47 % ± 1,0%, p < 0.01) and g__Odoribacter (1.31 % ± 0.7 % vs 0.30 % ± 0.2 %, p < 0.01). In addition, the development of CIC and abnormal lipid metabolism were significantly prevented in pseudo-germ-free mice. Therefore, we concluded CTS alleviated 5FU/CPT-11 induced colitis in CAC mice via regulating fecal flora associated lipid metabolism.

Dihydrotanshinone attenuates chemotherapy-induced intestinal mucositis and alters fecal microbiota in mice.

Chemotherapy-induced intestinal mucositis (CIM) is a principal reason for reduced living quality of patients undergoing chemotherapy. Growing evidence showed gut microbiota played an important role in the development of intestinal mucositis. Dihydrotanshinone I (DHTS) is a liposoluble extract of Salvia miltiorrhiza Bunge with many bioactivities. Here we investigated the effect of DHTS on intestinal mucositis induced by 5-fluorouracil and irinotecan in mice. We detected the degree of intestinal mucosal damage and inflammatory response in CIM mice with or without DHTS administration. The body weight and disease activity index (DAI) of mice were monitored each day. H&E staining was used to evaluate pathological damage. The contents of interleukin 6 (IL-6), tumor necrosis factor (TNFα), diacylglycerol (DAO) and triglyceride (TG) in serum were determined by commercial kits. We also investigated the changes of fecal microbiota by 16S rRNA high-throughput sequencing. Spearman correlation analysis was used to evaluate the correlation between fecal microbiota and inflammatory factors. Tax4Funwas performed to infer the potential function of the microbial community. Results showed DHTS significantly reduced DAI, intestinal mucosal damage and inflammatory response in CIM mice by decreasing serum IL-6 and TNFα. In addition, there is an intense correlation between fecal microbiota and inflammatory factors. DHTS efficiently reversed disordered fecal microflora close to normal and increased the abundance of g__Akkermansia. DHTS also enriched bacterial species which promote butyric acid metabolism or negatively correlated with inflammatory factors. Besides, species enriched by DHTS in fecal microbiota were probably involved in glutamine production and ammonia oxidation. In conclusion, our study provides evidence that DHTS effectively attenuates CIM induced by 5-fluorouracil and irinotecan in mice. Regulation of the composition and function of fecal microbiota probably plays a critical role in the therapeutic effect of DHTS in CIM mice.