cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.10156373
title: Data accompanying the manuscript "Assessing the Probability of Extremely Low Wind Energy Production in Europe at Sub-seasonal to Seasonal Time Scales"

description: This dataset contains time series of wind energy production aggregated over France and Europe, obtained from a 1000-year climate simulation from the CESM model (version 1.2.2, Hurrel et al. 2013), coupled to a simple energy model to compute grid-point capacity factor from surface wind. Wind power is then computed by multiplying the capacity factor by the installed capacity, taken from 5 e-Highway scenarios (X5, X7, X10, X13 and X16), and integrated over the regions of interest. More details about the climate simulation, wind energy model and installed capacity scenarios can be found in the associated manuscript, "Assessing the Probability of Extremely Low Wind Energy Production in Europe at Sub-seasonal to Seasonal Time Scales" (Cozian et al. 2023).
The data is organized into 10 files for France and 10 files for Europe. In each case, the 10 files correspond to 10 batches of 100 years each, with 3-hourly output. Each file contains 5 time series corresponding to the 5 installed capacity scenarios.
References

Hurrell J W, Holland M M, Gent P R, Ghan S, Kay J E, Kushner P J, Lamarque J F, Large W G, Lawrence D, Lindsay K, Lipscomb W H, Long M C, Mahowald N, Marsh D R, Neale R B, Rasch P, Vavrus S, Vertenstein M, Bader D, Collins W D, Hack J J, Kiehl J and Marshall S (2013). The community earth system model: A framework for collaborative research. Bulletin of the American Meteorological Society, 94, 1339–1360. https://doi.org/10.1175/BAMS-D-12-00121.1
e-Highway 2050 (2015). Europe's future secure and sustainable electricity infrastructure. https://docs.entsoe.eu/baltic-conf/bites/www.e-highway2050.eu/results
Cozian B, Herbert C and Bouchet F (2023). Assessing the Probability of Extremely Low Wind Energy Production in Europe at Sub-seasonal to Seasonal Time Scales. https://doi.org/10.48550/arXiv.2311.13526
DOI: 10.25824/redu/e9embk
title: relatorioIndig2.doc

description: Statistical Analysis
DOI: 10.25824/redu/doxrsn
title: relatorioIndig3.doc

description: Study Power
DOI: 10.25824/redu/jw9afm
title: 20221003_BancoIndig_Helymar_v2.xls

description: :unav
DOI: 10.25824/redu/9blfck
title: Cervical cancer screening in Brazilian Amazon indigenous women: an opportunity for the intensification of public policies for prevention.ira, de 2007 a 2019

description: Metadata of manuscript
DOI: 10.6084/m9.figshare.24624066
title: Longitude and latitude coordinates of G. sarpedon

description: Longitude and latitude coordinates of G. sarpedon
DOI: 10.25326/541
title: EXAEDRE-L2 SAETTA Science Data

description: Temporal and spatial measurements of the total (intra-cloud and cloud-to-ground) lightning activity based on the VHF radiation emitted by the lightning discharges.

EXAEDRE L2 SAETTA Science Data emanate from L1 SAETTA Science Data  with additional attributes including flash ID number. EXAEDRE L2 SAETTA Science Data have been produced for the 5-month period of the EXAEDRE Enhanced Observation Period (EOP) from June 2018 to October 2018.

L2 SAETTA Science Data files are stored per 10-min period in ASCII format. Each file contains the list of VHF sources that have been reconstructed from the signals measured at the 12 SAETTA stations deployed in Corsica. Each VHF source is described similarly to L1 SAETTA Science Data by its occurrence time, its latitude, its longitude, its altitude, its VHF power, a quality parameter (CHI2), and the list of SAETTA stations that contributed to the location computation of the VHF source. Additionally the number of SAETTA stations that contributed in the reconstruction of the source is given as well as the flash ID number to which flash the source belongs.

Note that the flash ID starts from 0 at each 10-min period.
DOI: 10.5281/zenodo.8337062
title: Primary NMR Data Supporting the Article "Synthetic approach to 2-alkyl-4-quinolones and 2-alkyl-4-quinolone-3-carboxamides based on common β-keto amide precursors"

description: This archive contains raw 1H/13C FIDs and associated data in Bruker-specific format that can be viewed with Bruker’s TopSpin or other appropriate NMR processing software. The subfolders are named in accordance with the compound numbering in the associated research paper (Synthetic Approach to 2-Alkyl-4-quinolones and 2-Alkyl-4-quinolone-3-carboxamides Based on Common β-Keto Amide Precursors).


Correspondence: angelov@uni-plovdiv.bg
DOI: 10.5281/zenodo.8337063
title: Primary NMR Data Supporting the Article "Synthetic approach to 2-alkyl-4-quinolones and 2-alkyl-4-quinolone-3-carboxamides based on common β-keto amide precursors"

description: This archive contains raw 1H/13C FIDs and associated data in Bruker-specific format that can be viewed with Bruker’s TopSpin or other appropriate NMR processing software. The subfolders are named in accordance with the compound numbering in the associated research paper (Synthetic Approach to 2-Alkyl-4-quinolones and 2-Alkyl-4-quinolone-3-carboxamides Based on Common β-Keto Amide Precursors).


Correspondence: angelov@uni-plovdiv.bg
DOI: 10.6084/m9.figshare.24523342
title: Supplementary Material for: Clinical effects of oral supplementation of gamma-ciclodextrin curcumin complex in male patients with moderate-to-severe BPH-related Lower Urinary Tract Symptoms

description: Introduction: Benign prostatic hyperplasia (BPH) is the most common cause of lower urinary tract symptoms (LUTS) in males. Curcumin exhibits anti-inflammatory and anti-tumor properties which may be effective for BPH. This multi-arm observational study evaluated the real-world efficacy of QURMIN® (Gamma-cyclodextrin-curcumin Complex-CAVACURMIN®) as single or combination therapy for BPH. Methods: Men with moderate-severe LUTS/BPH receiving a 6-month supplementation with QURMIN® alone or in combination with BPH-specific medication were propensity score matched with patients not taking curcumin and then divided into subgroups based on concomitant baseline treatment. Cohorts were compared in the 6-month variation of IPSS, quality of life (IPSS-QoL), Benign prostatic Hyperplasia Impact Index (BII) and uroflowmetry parameters. Curcumin tolerability was evaluated in terms of discontinuations and adverse effects. Results: The 1:1 propensity score matching resulted in a treatment-naïve (n=152), an alpha-blocker only(AB)(n=138) and a AB+5-alpha reductase inhibitors (5-ARI) (n=78) subgroup. After 6 months, drug-naïve patients taking curcumin reported significant improvement in IPSS-storage (-3.9,p&lt;0.001), IPSS-voiding(-2.0,p=0.011), IPSS-total(-5.9,p&lt;0.001), IPSS-QoL(-3.9,p&lt;0.001), BII(-2.0,p&lt;0.001), Qmax(+3.1 ml/s,p&lt;0.001), Qmean(+1.9 ml/s,p=0.005), PVR(-7.7 ml,p&lt;0.001), and PSA(-0.3 ng/ml,p=0.003), compared to controls. Patients taking ABs and curcumin showed improvement in IPSS-storage(-2.7,p&lt;0.001), IPSS-voiding(-1.3,p=0.033), IPSS-total(-3.5,p&lt;0.001), IPSS-QoL(-1.1,p=0.004), BII(-1.7,p=0.006), Qmax(+1.0 ml/s,p=0.006) and PSA(-0.2 ng/ml,p=0.01). Patients taking curcumin and AB+5-ARI showed improvement in IPSS-storage(-1.3,p=0.007), IPSS-total(-1.6,p=0.034), IPSS-QoL(-1.1,p&lt;0.001) and BII(-2.0,p&lt;0.001). No adverse reactions were reported for curcumin supplementation. Conclusion: QURMIN® (CAVACURMIN®) led to significant improvements in symptom burden, uroflow parameters and QoL, without significant additional side effects, thus proving to be a potential new treatment for BPH, either as a single therapy or in addition to standard treatment.
DOI: 10.6084/m9.figshare.24523342.v1
title: Supplementary Material for: Clinical effects of oral supplementation of gamma-ciclodextrin curcumin complex in male patients with moderate-to-severe BPH-related Lower Urinary Tract Symptoms

description: Introduction: Benign prostatic hyperplasia (BPH) is the most common cause of lower urinary tract symptoms (LUTS) in males. Curcumin exhibits anti-inflammatory and anti-tumor properties which may be effective for BPH. This multi-arm observational study evaluated the real-world efficacy of QURMIN® (Gamma-cyclodextrin-curcumin Complex-CAVACURMIN®) as single or combination therapy for BPH. Methods: Men with moderate-severe LUTS/BPH receiving a 6-month supplementation with QURMIN® alone or in combination with BPH-specific medication were propensity score matched with patients not taking curcumin and then divided into subgroups based on concomitant baseline treatment. Cohorts were compared in the 6-month variation of IPSS, quality of life (IPSS-QoL), Benign prostatic Hyperplasia Impact Index (BII) and uroflowmetry parameters. Curcumin tolerability was evaluated in terms of discontinuations and adverse effects. Results: The 1:1 propensity score matching resulted in a treatment-naïve (n=152), an alpha-blocker only(AB)(n=138) and a AB+5-alpha reductase inhibitors (5-ARI) (n=78) subgroup. After 6 months, drug-naïve patients taking curcumin reported significant improvement in IPSS-storage (-3.9,p&lt;0.001), IPSS-voiding(-2.0,p=0.011), IPSS-total(-5.9,p&lt;0.001), IPSS-QoL(-3.9,p&lt;0.001), BII(-2.0,p&lt;0.001), Qmax(+3.1 ml/s,p&lt;0.001), Qmean(+1.9 ml/s,p=0.005), PVR(-7.7 ml,p&lt;0.001), and PSA(-0.3 ng/ml,p=0.003), compared to controls. Patients taking ABs and curcumin showed improvement in IPSS-storage(-2.7,p&lt;0.001), IPSS-voiding(-1.3,p=0.033), IPSS-total(-3.5,p&lt;0.001), IPSS-QoL(-1.1,p=0.004), BII(-1.7,p=0.006), Qmax(+1.0 ml/s,p=0.006) and PSA(-0.2 ng/ml,p=0.01). Patients taking curcumin and AB+5-ARI showed improvement in IPSS-storage(-1.3,p=0.007), IPSS-total(-1.6,p=0.034), IPSS-QoL(-1.1,p&lt;0.001) and BII(-2.0,p&lt;0.001). No adverse reactions were reported for curcumin supplementation. Conclusion: QURMIN® (CAVACURMIN®) led to significant improvements in symptom burden, uroflow parameters and QoL, without significant additional side effects, thus proving to be a potential new treatment for BPH, either as a single therapy or in addition to standard treatment.
DOI: 10.25625/cjc193/nzwuub
title: R1-Fig S8 -EMPA correlation 3.jpg

description: Figure S8. FeO-SiO2 and Sr(ppm)-Mg(mol%) correlations of the selected samples from NR1003 drill core by electron microprobe analysis.
DOI: 10.25625/cjc193/ymawxi
title: FIgure 8-Model single column-Siltingup effect-low H2S analcime.jpg

description: Fig. 8. Models of carbonate formation coupled with hydrochemistry and biogeochemistry. A1, B1, C1 and D1: scenarios of carbonate-poor beds due to lower salinity; A2, B2, C2, D2: scenarios of intensive carbonate formation (carbonate-rich beds) due to high salinity. A). The early Ries crater lake (clinoptilolite smbr) with a high sulfate level due to sulfate-rich groundwaters discharged from the crystalline basement. More Ca-rich dolomite is present in A2 than in the carbonate-poor bed (A1). The subsequent phase is characterized by a large lake volume and decreased salinity (analcime smbr, B). Note that 1) no major methanogenesis is evident in A and B; 2) considerable dissolved iron was present in B; 3) a presumed lower sulfate concentration in B as indicated by width of the sulfate curve than A. B1: marcasite and siderite formed at the time of the carbonate-poor interval; B2: ankerite and Ca-rich dolomite formed during the interval of intensive carbonate formation, as a result of high iron availability in porewaters. C) As ongoing iron and sulfate reduction further led to a low-sulfate interval, methanogenesis started and resulted in an enriched 13C DIC (high δ13C interval). Episodical inflow derived from Bunte Breccia and recurring stratification caused fluctuating physio-chemical conditions, facilitating Ostwald’s ripening process to promote dolomite formation in high 13C DIC environments. C1: in the carbonate-poor interval, biogenic primary calcites and Ca-rich dolomite formed, and small framboidal pyrites (&lt;5μm) formed in the water column; C2: at the time of intensive carbonate formation, Ca-rich dolomite formed following an increase in salinity. D) Following the lake level drop, dissolved oxygen reached the lake bottom and caused a downward shift of the anaerobic zone (dolomite-marl smbr and upper clay member). MOX: aerobic methanotrophy. D1: framboidal pyrites (&gt;5μm) formed in sediments during a carbonate-poor interval; D2: Ca-rich dolomite and calcite precipitated at a time of intensive carbonate formation.
DOI: 10.25625/cjc193/h9bbi0
title: R1-Fig S9 Stot-d13C correlation.JPG

description: Figure S9. Correlation plot between S tot and δ13C of samples from the high δ13C interval.
DOI: 10.25625/cjc193/vlohbu
title: Figure 4 Columnar section geochemistry.jpg

description: Fig. 4. Element ratios (Si/Al, K/Al, Zr/Al and Ba/Al) from bulk μ-XRF elemental analyses (Table S8) of the carbonate-bearing marlstone samples.
DOI: 10.25625/cjc193/5kgzyc
title: R1-Fig S5 -Biomarker structure.jpg

description: Figure S5. Structures of the selected organic compounds detected from the NR1003 drill core.
DOI: 10.25625/cjc193/nqbgqp
title: R1-Fig S7 -EMPA correlation 2.jpg

description: Figure S7. FeO-SiO2 and Sr(ppm)-Mg(mol%) correlations of the selected samples from NR1003 drill core by electron microprobe analysis.
DOI: 10.25625/cjc193/ag1lpp
title: R1-Fig S4 EMPA 2.jpg

description: Figure S4. Photomicrographs of carbonates from the Miocene Ries crater lake. A: close-up of a marlstone sample (bulk δ13C = +5.51‰, δ18O = +0.70‰) in the high δ13C interval, containing medium-grey Ca-rich dolomite and white-grey siderite. Siderites (white squares) are euhedral to subeuhedral, often with etched surfaces and twinning edges (white arrows). B: close-up of the marlstone sample that shows framboidal pyrites (bulk δ13C = +6.97‰, δ18O = +0.33‰), which were detected for the first time from downcore to top (NR1003-164, 131.6 m core depth). Note the submicrometer Ca-rich dolomite (black arrows) and white-grey thin, linear structure resembling extracelluar polymeric substance (EPS, white arrow). C: zoom-out of the marlstone sample (NR1003-8, bulk δ13C = +17.03‰, δ18O = +2.12‰, 121.6 m core depth), showing dolomite-poor, bioclast-rich lamina between the white dashed line and dolomite-rich laminae outside the dashed line. Note that the bioclast is encrusted by Ca-rich dolomites (EPS?). For dolomite-rich laminae, Ca-rich dolomites form thicker sheaths (white arrows) than the bioclast-rich lamina (black arrows). D: close-up of Ca-rich dolomite sheaths (white arrows) and disordered Ca-rich dolomite cores (black arrows) inside the biogenic tube structures (147.8 m core depth, bulk δ13C = +12.94‰, δ18O = +3.88‰). E: rhombohedral stoichiometric dolomite (98.1 m core depth, bulk δ13C = +16.40‰, δ18O = +0.28‰). F: white-grey submicrometer-sized Ca-rich dolomite and calcified green algae (white arrows) at 74.4 core depth (bulk δ13C = +6.99‰, δ18O = +1.38‰). F: subeuhedral to euhedral Ca-rich dolomites, filling the pore spaces between smectites. White arrows refer framboidal pyrites (38.9 core depth, bulk δ13C = +2.46‰, δ18O = +0.32‰). G: rhombohedral Ca-rich dolomites and framboidal pyrites (white square, 33.3 m core depth, bulk δ13C = +0.94‰, δ18O = -0.30‰).
DOI: 10.25625/cjc193/3h9h7e
title: Figure 2. Columnar section.jpg

description: Fig. 2. Sedimentary profile of the NR1003 drill core and profiles of carbonate contents in different phases (left), stable carbon and oxygen isotopes (right). Clay, marl (or dolomite marl) and limestone (or dolostone) are defined by &lt;25% CaCO3, 25–75% CaCO3, &gt;75% CaCO3 (or equivalent CaMg(CO3)2). Likewise, the microcrystalline calcite, calcite-rich mixture, dolomite-rich mixture and microcrystalline dolomite are defined by &gt;75 mol% calcite, 50-75 mol % calcite, 50–75 mol % dolomite and &gt;75 mol % dolomite. See Table S3 for detailed Ccarb and Table S4 and S5 for XRD data, Table S6 for stable isotope data. Note that the dolomite in the left column refers to the calculated dolomite content, on basis of Ccarb and relative intensity of dolomite peak (hkl 104) in XRD patterns (Table S4). Only dolomite (i.e. no subdivision between ferroan and Ca-rich dolomite) is shown here (see 3.3). The age of the volcanic ash layer is derived from Arp et al. (2021).
DOI: 10.25625/cjc193/99ko1x
title: Appendix B. Research Data.tab

description: :unav
DOI: 10.25625/cjc193/wepmyx
title: R1-Fig S3 EMPA photomicrographs.jpg

description: Figure S3. Photomicrographs of carbonates in the Miocene Ries crater lake. A: close-up of a laminated marlstone from the basal member, with light-colored calcite laminae and dark-colored dolomite-rich laminae. Note the higher smectite/siliciclastic contents in the dolomite-rich laminae. B: close-up of calcites and dolomite from the basal member. Note some core or zonation is shown in the dark colored subeuhedral dolomite. C: close-up of Ca-rich dolomites from the clinoptilolite smbr. Note that most dolomites are surrounded by smectites and some submicrometer euhedral dolomites formed in interstitial spaces (white square). D: Ca-rich dolomite (Ca-dol), ankerite (ank) and iron sulfide/monosulfide (is) at the analcime smbr. Note that some Ca-rich dolomite and ankerite formed at the rim of iron sulfide. E: round or subround pellets (40 – 60 µm wide), filled with Ca-rich dolomites. F: mosaiced Ca-rich dolomite, ankerite (white rectangle) and submicrometer euhedral Ca-rich dolomite ininterstitial spaces. G: concretion of chalcedony (q: quartz) at the analcime smbr, whose outer rim is partly replaced by twinning-spearheaded marcasite (m, e.g. Schieber, 2011). H: 30-µm-sized siderite (sid) aggregate.
DOI: 10.25625/cjc193/kztzkr
title: Table 1 biomarker-sources-and-environment .tab

description: Table 1. Selected biomarkers, their biological sources and environmental indications.
DOI: 10.25625/cjc193/qyiws4
title: Figure 1 Geological map with volcanic ash layer.jpg

description: Fig. 1. Geographical and geological overview of the Ries impact structure (based on Ernstson, 1974; Pohl et al., 1977; Hüttner and Schmidt-Kaler, 1999) and location of the drilling sites Nördlinger Ries 1003 (NR1003) and Nördlingen 1973. Lithostratigraphic subdivision of the sedimentary crater fill based on Jankowski (1981). For exact occurrence of volcanic ash layer in the lake deposits, readers are referred to Arp et al. (2021).
DOI: 10.25625/cjc193/yj0hog
title: Table 2 biomakers-with-concentration .tab

description: Concentrations of selected biomarkers. Note that ‘TOC’ refers to C org (wt%) of the carbonate-free samples (i.e. residues after decarbonation). i/ai-C15:0: sum concentration of iso- and anteiso-pentadecanoic acids.
DOI: 10.25625/cjc193/lhe3us
title: R1-Fig S1 lithofacies +fossils.jpg

description: Figure S1 Different lithofacies and fossils from drill core NR 1003. A: Conglomerate and coarse-grained pebbly sandstone in the basal member (242.0 to 242.8 m depth), containing pebbles reworked from crystalline basement rocks of the inner ring. B: Well-preserved fish from the laminite member (diatom subunit, 106 m depth). C: Artemia faecal pellets from laminite member (clinoptilolite subunit, 216.6 m depth). D: Dark grey to black stratified lignite with elemental sulphur from present-day sulfide oxidation. E: Pedoturbation/pedogenic slickenside in the dark grey and ochre-brown mottling carbonaceous claystone (clay member, 22.0 to 22.2 m depth). F. Hydrobia trochulus and shell debris from the clay member (38.4 m depth). G. Gyraulus and shell debris from clay member (30.26 m depth). H: Compressed shell debris of Planorbarius (clay member, 32.0 m depth). I: Desiccation crack with in-situ brecciation (clay member, 32.1 m depth).
DOI: 10.25625/cjc193/1sqtyd
title: R1-Fig S6 -EMPA correlation 1.jpg

description: Figure S6. FeO-SiO2 and Sr(ppm)-Mg(mol%) correlations of the selected samples from NR1003 drill core (continued in Figure S7) by electron microprobe analysis. When Fe and Mn do not show any correlation with Si, Fe and Mn are considered as incorporated into the carbonate lattice. Note that different carbonate phases are well separated into different zones in Sr(ppm)-Mg(mol%) plots.
DOI: 10.25625/cjc193/iyrztu
title: R1-Fig S2 Basal member lithology.jpg

description: Figure S2. Core image of carbonate-bearing section in the basal member. The laminated marlstone with fluid escape structures between 242.41 to 243.7 m is typical for upper part of sedimentary cycle in the basal member. Between 238.4 to 242.41 m comprises the lower-middle part of the cycle, which contain pebbly sandstone/fine-grained conglomerate to fine-grained calcareous sandstone or calcareous siltstone.
DOI: 10.25625/cjc193/kz6ke2
title: Appendix A Supplementary figures.docx

description: :unav
DOI: 10.25625/cjc193/lrkfqx
title: R1-Fig S10 -High d13C interval C-O-Ccarb.jpg

description: Figure S10. Correlation plots between δ13C, δ18O values and bulk carbonate contents (C carb) in dolomite and dolomite-rich samples from the high δ13C interval. The moderate to strong covariations between δ13C and δ18O values can be explained by coupled short-term hydrological and biogeochemical variations. When the freshwater influx was lower, the water body became more stagnant and saline (consequently higher δ18O values), thus facilitating anaerobic respiration and scavenging inhibitors for methanogenesis (e.g., sulfate). These processes led to the high δ13C values in the dolomite-rich samples. At times of higher freshwater influxes, dolomite formation ceases due to a lower cation concentration in the porewater, whereas a greater amount of low-δ18O calcites form from water column. The δ13C values of these calcites mainly reflect evaporation and photosynthesis effects from lake surface. While minor dolomites still form in the stratified lake bottom with higher 13C DIC, intermediate bulk δ18O-δ13C values are found in dolomite-calcite mixtures (Table S6). Shallow burial or late diagenetic events do not explain the observations.
DOI: 10.25625/cjc193/kzatuj
title: Figure 6 Isotope covariation_Ries_New_Figure_v2.jpg

description: Fig. 6. Stable carbon–oxygen covariation plots of the samples from the laminated marlstone section (226 to 87.3 m core depth). A: samples from the high δ13C interval (upper laminite member and varicolored smbr, symbols with black outlines), analcime smbr (red-outlined symbols) and clinoptilolite smbr (purple-outlined symbols); note that most of the samples are dolomites. The covariation trend line is calculated based on calcite and calcite-rich mixture samples from clinoptilolite to varicolored-marl smbr. B: Calcite and calcite-rich samples from NR1003 (black symbols) and Nördlingen 1973 (grey-filled symbols, Rothe and Hoefs, 1977); Miocene (pre-impact) floodplain carbonate (blue-outlined and yellow-filled symbols) at Pleinfeld locality, ca. 30 km away from the Ries crater (Zeng et al., 2021) and with their mean δ18O values representing the meteoric calcite line.
DOI: 10.25625/cjc193/cbko3t
title: Figure 7 high-d13C-dolomite-Ries-1.jpg

description: Fig. 7. Interpretations of pore water biogeochemical processes, lake physiochemistry and solute provenance of the Ries crater lake based on observations from this study. TSR: thermochemical sulfate reduction; MSR: microbial sulfate reduction; MOX: aerobic methane oxidation. The gypsum pseudomorphs in the clay member were reported by Arp et al. (2017) and in basal member by Jankowski (1981); thiophenes in clinoptilolite smbr was reported by Barakat and Rullk¨otter (1997) otherwise in this study; occurrences of diatoms by (Schauderna, 1983). The estimated lake level curve is based on sedimentological observations (e.g. lamination, bioturbation, slumping, mud cracks, in-situ brecciation) in this study and diatom associations in drill core N¨ordlingen 1973 (Schauderna, 1983). The estimated salinity was depicted schematically from indicative organic compounds (Zhao et al., 2022a). The δ15N values schematically correlate with lake water pH variations, with support from hydrochemical modeling results (Stüeken et al., 2020). S isotope data of sedimentary sulfides from drill core N¨ordlingen 1973 were adopted and modified from Tino et al. (2023).