cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.710915
title: (Table 1) Mineralogy of oceanic crust from ODP Hole 153-923A
DOI: 10.1594/pangaea.805786
title: (Appendix A -Table 3) Geochemistry at DSDP Hole 82-559

description: Sediment depth is given in mbsf. All samples belong to Chemical Group I.
DOI: 10.1594/pangaea.793361
title: (Table 6) Normative composition at DSDP Hole 89-462A

description: Sediment depth is given in mbsf. Calculated on anhydrous, carbonate-free basis and an Fe2O3/FeO of 0.15.
DOI: 10.1594/pangaea.229925
title: Sound velocity of Hole 89-586A
DOI: 10.1594/pangaea.229926
title: Sound velocity of Hole 89-586B
DOI: 10.1594/pangaea.380604
title: Radiosonde PS14/10534 during POLARSTERN cruise ANT-VII/1 on 1988-09-20 22:00h

description: Height of tropopause 14878 m, precipitable water content 2.0423 cm, total ozone 278.3 DU
DOI: 10.1594/pangaea.879428
title: Upwelling spectral radiance as measured in different depths at radiometer station PS73/013-2 (corrected version)

description: In the previous upwelling radiance (Lu) profile data set (doi:10.1594/PANGAEA.820795), Lu data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement). The results of the publications related to these data were not affected. Taylor et al. 2013 investigated only Lu data incorrectly shifted by 3 nm, so the analysis was consistent within itself. Taylor et al. 2011 and Bracher et al. 2015 used the remote sensing reflectance (RRS) data calculated from the incorrectly shifted Lu data. The resulting RRS data only showed inconsistencies were the incoming downwelling irradiance changes quickly with wavelengths, which resulted erroneous features &lt;430 nm. We have used both versions (previous and the one presented here) Lu and RRS data and got the same results since the wrong features &lt;430 nm are consistent and are neither used for the hierarchical cluster analysis (only data &gt;430 nm are considered) performed in Taylor et al. 2011 nor for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015.
DOI: 10.1594/pangaea.776106
title: (Tabelle T4) Oxygen isotopic composition of interstitial waters from ODP Site 207-1260 sediments

description: Depth, sediment is given in mbsf. Measurement precision based on replicate measurements of standards was 0.03 per mil (1 sigma).
DOI: 10.1594/pangaea.419850
title: Hourly delayed mode sea level from coastal tide gauge station Key_West in 1990
DOI: 10.1594/pangaea.231138
title: Smear slide analysis of Hole 86-577B
DOI: 10.1594/pangaea.419808
title: Hourly delayed mode sea level from coastal tide gauge station Key_West in 1934
DOI: 10.1594/pangaea.419822
title: Hourly delayed mode sea level from coastal tide gauge station Key_West in 1948
DOI: 10.1594/pangaea.419844
title: Hourly delayed mode sea level from coastal tide gauge station Key_West in 1984
DOI: 10.1594/pangaea.810600
title: (Table 2) Chemical compositions of Plagioclase in basalts at DSDP Leg 74 Holes
DOI: 10.1594/pangaea.231139
title: Smear slide analysis of Hole 86-578
DOI: 10.1594/pangaea.775920
title: (Table T2) Diatoms in sediments of ODP Hole 207-1257B

description: Floral notes: Mostly fragments of diatoms and radiolarians. Diatom species include Cosciondiscus excavatus v. quadriocellata, C. marginatus, Asterolampra praemarylandica, Trinacria sp., Cestodiscus convexus, and C. trochus.
DOI: 10.1594/pangaea.747732
title: (Table 3) Carbon concentrations of ODP Hole 110-672A
DOI: 10.1594/pangaea.689660
title: Radiosonde M49_R284 during METEOR cruise M49 on 1978-08-29 14:29h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.15468/dl.778j7k
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((148.147168 -33.925572, 148.147168 -33.930063, 148.151659 -33.930063, 148.151659 -33.925572, 148.147168 -33.925572))"
 ]
}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069963-240626123714530/datasets/export for details.
DOI: 10.6084/m9.figshare.24546944
title: Additional file 1 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 1: Table S1. Differences in TE subfamily cis-regulatory activities estimated by craTEs across experiments presented in Fig. 1C.
DOI: 10.6084/m9.figshare.24546944.v1
title: Additional file 1 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 1: Table S1. Differences in TE subfamily cis-regulatory activities estimated by craTEs across experiments presented in Fig. 1C.
DOI: 10.6084/m9.figshare.24547038
title: Additional file 2 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 2: Table S2. Enriched TE subfamilies found in the proximity of differentially expressed (DE) genes for LTR5-Hs/SVA CRISPRi g#1 using lenient DE calling (Fisher’s exact test, p-val [MYLT]0.05). The sign of the log fold change (up/downregulation) is reported in the “direction” column. DE genes were called without adjusting for multiple testing. p-values for the enrichment test were computed according to the hypergeometric distribution, and adjusted with the Benjamini-Hochberg procedure.
DOI: 10.6084/m9.figshare.24547038.v1
title: Additional file 2 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 2: Table S2. Enriched TE subfamilies found in the proximity of differentially expressed (DE) genes for LTR5-Hs/SVA CRISPRi g#1 using lenient DE calling (Fisher’s exact test, p-val [MYLT]0.05). The sign of the log fold change (up/downregulation) is reported in the “direction” column. DE genes were called without adjusting for multiple testing. p-values for the enrichment test were computed according to the hypergeometric distribution, and adjusted with the Benjamini-Hochberg procedure.
DOI: 10.6084/m9.figshare.26638248
title: Additional file 3 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 3: Table S3. Enriched TE subfamilies found in the proximity of differentially expressed (DE) genes for LTR5-Hs/SVA CRISPRi g#1 using stringent DE calling (Fisher’s exact test, BH-adjusted p-val [MYLT]0.05).
DOI: 10.6084/m9.figshare.26638248.v1
title: Additional file 3 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 3: Table S3. Enriched TE subfamilies found in the proximity of differentially expressed (DE) genes for LTR5-Hs/SVA CRISPRi g#1 using stringent DE calling (Fisher’s exact test, BH-adjusted p-val [MYLT]0.05).
DOI: 10.6084/m9.figshare.26638251
title: Additional file 4 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 4: Table S4. TE subfamilies enriched for increased and/or decreased ATAC-seq peaks for LTR5-Hs/SVA CRISPRi g#1.
DOI: 10.6084/m9.figshare.26638251.v1
title: Additional file 4 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 4: Table S4. TE subfamilies enriched for increased and/or decreased ATAC-seq peaks for LTR5-Hs/SVA CRISPRi g#1.
DOI: 10.6084/m9.figshare.26638254
title: Additional file 5 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 5: Table S5. TE subfamilies enriched for increased and/or decreased ATAC-seq peaks for LTR5-Hs/SVA CRISPRi g#2.
DOI: 10.6084/m9.figshare.26638254.v1
title: Additional file 5 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 5: Table S5. TE subfamilies enriched for increased and/or decreased ATAC-seq peaks for LTR5-Hs/SVA CRISPRi g#2.
DOI: 10.6084/m9.figshare.26638257
title: Additional file 6 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 6: Table S6. TE subfamilies enriched for increased and/or decreased H3K9me3 ChIP-seq peaks for LTR5-Hs/SVA CRISPRi g#2.
DOI: 10.6084/m9.figshare.26638257.v1
title: Additional file 6 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 6: Table S6. TE subfamilies enriched for increased and/or decreased H3K9me3 ChIP-seq peaks for LTR5-Hs/SVA CRISPRi g#2.
DOI: 10.6084/m9.figshare.26638260
title: Additional file 7 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 7: Table S7. Estimated cis-regulatory activities for the TE subfamilies and transgene overexpression experiments underlying Figs. 3A and S4.
DOI: 10.6084/m9.figshare.26638260.v1
title: Additional file 7 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 7: Table S7. Estimated cis-regulatory activities for the TE subfamilies and transgene overexpression experiments underlying Figs. 3A and S4.
DOI: 10.6084/m9.figshare.26638263
title: Additional file 8 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 8. Related to Fig. 3. Contains estimated TE subfamily activities for the RNA-seq dataset of transgene overexpression in hESCs [47] in .csv format, available at URL: https://doi.org/10.5281/zenodo.8116824 . Title of data: Transposable element (TE) subfamily cis-regulatory activities estimated from 441 transgene overexpression experiments in human embryonic stem cells (hESCs). Description of data: Activities were estimated using craTEs with the weighted susceptibility matrix N computed with $$L = 2.5e5kB$$ L = 2.5 e 5 k B . Rows are transposable element (TE) subfamilies, columns are as follows: $$\cdot$$ · Estimate: estimated cis-regulatory activity, correponds to a linear regression coefficient. $$\cdot$$ · Std. Error: standard error of linear regression coefficient. $$\cdot$$ ·  t value: t value corresponding to t-test with H0: Estimate = 0 and HA: Estimate $$\ne$$ ≠ 0. $$\cdot$$ ·   $$Pr(&gt;|t|)$$ P r ( &gt; | t | ) : probability (p-value) of observing a more extreme t value. $$\cdot$$ · p_adj: p-values adjusted with the Benjamini Hochberg procedure. $$\cdot$$ · TE: TE subfamily. $$\cdot$$ · condition: concatenation of the name of the overexpressed transgene and the timepoint. $$\cdot$$ · transgene: symbol for the overexpressed transgene. $$\cdot$$ · timepoint: time under transgene induction via DOX treatment.
DOI: 10.1594/pangaea.744952
title: Basic measurements of radiation at station Chesapeake Light (2010-08)
DOI: 10.6084/m9.figshare.26638263.v1
title: Additional file 8 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 8. Related to Fig. 3. Contains estimated TE subfamily activities for the RNA-seq dataset of transgene overexpression in hESCs [47] in .csv format, available at URL: https://doi.org/10.5281/zenodo.8116824 . Title of data: Transposable element (TE) subfamily cis-regulatory activities estimated from 441 transgene overexpression experiments in human embryonic stem cells (hESCs). Description of data: Activities were estimated using craTEs with the weighted susceptibility matrix N computed with $$L = 2.5e5kB$$ L = 2.5 e 5 k B . Rows are transposable element (TE) subfamilies, columns are as follows: $$\cdot$$ · Estimate: estimated cis-regulatory activity, correponds to a linear regression coefficient. $$\cdot$$ · Std. Error: standard error of linear regression coefficient. $$\cdot$$ ·  t value: t value corresponding to t-test with H0: Estimate = 0 and HA: Estimate $$\ne$$ ≠ 0. $$\cdot$$ ·   $$Pr(&gt;|t|)$$ P r ( &gt; | t | ) : probability (p-value) of observing a more extreme t value. $$\cdot$$ · p_adj: p-values adjusted with the Benjamini Hochberg procedure. $$\cdot$$ · TE: TE subfamily. $$\cdot$$ · condition: concatenation of the name of the overexpressed transgene and the timepoint. $$\cdot$$ · transgene: symbol for the overexpressed transgene. $$\cdot$$ · timepoint: time under transgene induction via DOX treatment.
DOI: 10.6084/m9.figshare.26638269
title: Additional file 10 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 10. Related to Fig. 4 and Fig. S6. Contains the consensus sequences found under regions with high EOMES or GATA6 ChIP-seq coverage [70] at functional TE subfamilies in differentiating endodermal cells.
DOI: 10.6084/m9.figshare.26638269.v1
title: Additional file 10 of Statistical learning quantifies transposable element-mediated cis-regulation

description: Additional file 10. Related to Fig. 4 and Fig. S6. Contains the consensus sequences found under regions with high EOMES or GATA6 ChIP-seq coverage [70] at functional TE subfamilies in differentiating endodermal cells.
DOI: 10.1594/pangaea.775910
title: (Table T2) Silicoflagellate abundance in ODP Hole 207-1258A sediments
DOI: 10.1594/pangaea.775919
title: (Table T1) Diatoms in ODP Leg 207 sediments
DOI: 10.1594/pangaea.419296
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1995
DOI: 10.1594/pangaea.419264
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1963
DOI: 10.1594/pangaea.419273
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1972
DOI: 10.1594/pangaea.419277
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1976
DOI: 10.1594/pangaea.419279
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1978
DOI: 10.15468/dl.3qw7rk
title: Occurrence Download

description: A dataset containing 314 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is one of (Crudia zenkeri Harms)"
 ]
}

 The dataset includes 314 records from 27 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069964-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.419288
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1987
DOI: 10.1594/pangaea.419248
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1947
DOI: 10.1594/pangaea.419249
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1948
DOI: 10.1594/pangaea.419251
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1950
DOI: 10.1594/pangaea.419254
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1953
DOI: 10.1594/pangaea.419260
title: Hourly delayed mode sea level from coastal tide gauge station Halifax in 1959
DOI: 10.1594/pangaea.844703
title: Radiosonde PS90/37117 during POLARSTERN cruise PS90 (ANT-XXX/3) on 2015-03-02 11:00h

description: Height of tropopause 13394 m, precipitable water content 2.0539 cm
DOI: 10.1594/pangaea.904796
title: Carbonate scenarios analysis from different sources of Fluid inclusions, CCD reconstruction and boron isotopic seawater reconstructions (Fluid inclusions, CCD, RH13 d11Bsw)

description: Carbonate scenario analysis from Horita et al (2002) Fluid inclusions, Palike et al. (2012) CCD reconstruction and various boron isotopic seawater reconstructions.
DOI: 10.1594/pangaea.784462
title: Radiosonde PS79/32642 during POLARSTERN cruise ANT-XXVIII/1 on 2011-10-31 11:10h

description: Height of tropopause 10957 m, precipitable water content 2.5396 cm
DOI: 10.1594/pangaea.249402
title: Nannofossil abundance of Hole 6-59B

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.884219
title: Geochemistry at BIGO station M107_630-1 on given timesteps

description: Parameter 6 Barium --&gt; Boron
DOI: 10.1594/pangaea.696101
title: (Table 3) Plio-Pleistocene age-depth points of ODP Site 162-982 in the Southern Ocean

description: Depth is composite depth (mcd). The chronology was derived by correlation of the benthic foraminiferal oxygen isotopic signals with DSDP Site 94-607 (Raymo et al., 1990 doi:10.1016/0012-821X(90)90051-X) using the program Analyseries (Paillard et al., 1996 doi:10.1029/96EO00259)
DOI: 10.1594/pangaea.920286
title: Continuous water level observations at station BEFmate_I3upp (2017-06)
DOI: 10.1594/pangaea.920299
title: Continuous water level observations at station BEFmate_I3upp (2018-07)
DOI: 10.1594/pangaea.920309
title: Continuous water level observations at station BEFmate_I4low (2017-12)
DOI: 10.1594/pangaea.920326
title: Continuous water level observations at station BEFmate_I4pio (2017-07)
DOI: 10.1594/pangaea.139154
title: Physical properties of sediment core GIK23414-8
DOI: 10.1594/pangaea.774773
title: Kaolinite/chlorite ratios measured on sediment core PS2564-3
DOI: 10.1594/pangaea.418827
title: Hourly delayed mode sea level from coastal tide gauge station Duck in 1984
DOI: 10.1594/pangaea.711215
title: (Table 3) Calcium isotopic composition of Orbulina universa from ODP Site 154-925
DOI: 10.1594/pangaea.418830
title: Hourly delayed mode sea level from coastal tide gauge station Duck in 1987
DOI: 10.1594/pangaea.418832
title: Hourly delayed mode sea level from coastal tide gauge station Duck in 1989
DOI: 10.1594/pangaea.787792
title: (Table T9) Mass accumulation rates and bulk density of ODP Hole 173-1069A
DOI: 10.1594/pangaea.835669
title: Porewater geochemistry of sediment core MSM17/4_584
DOI: 10.1594/pangaea.778813
title: Basic measurements of radiation at station Chesapeake Light (2012-03)
DOI: 10.1594/pangaea.757726
title: (Table 3) Concentration of chlorinated hydrocarbons in certain hydrobionts, North Atlantic, 1984
DOI: 10.1594/pangaea.854770
title: Fig. 5 End member proportions of grain size analysis at Hole 162-983A
DOI: 10.1594/pangaea.314645
title: Continuous thermosalinograph oceanography along cruise track M28/2
DOI: 10.1594/pangaea.536191
title: Summary of ecologically and stratigraphically important foraminifera in surface samples of the NW African continental margin (Table 3)
DOI: 10.1594/pangaea.435694
title: Hourly sea level from coastal tide gauge station Lagos in 1968 (Research quality database)
DOI: 10.1594/pangaea.755236
title: (Table 4) Vertical distribution of biomass of age stages of Metridia pacifica in the Sea of Japan at Station VITYAZ7519
DOI: 10.1594/pangaea.435532
title: Hourly sea level from coastal tide gauge station Key_West in 1959 (Research quality database)
DOI: 10.1594/pangaea.884199
title: Porewater geochemistry of sediment core M107_583-1

description: Second Barium parameter --&gt; Boron
DOI: 10.1594/pangaea.435525
title: Hourly sea level from coastal tide gauge station Key_West in 1923 (Research quality database)
DOI: 10.1594/pangaea.783679
title: Basic measurements of radiation at station Chesapeake Light (2012-05)
DOI: 10.1594/pangaea.902715
title: (Table S10) 230Th-normalized age model of sediment core SU90-03
DOI: 10.1594/pangaea.902717
title: Sea surface temperature reconstruction of sediment core SU90-08 over the last 40 ka
DOI: 10.1594/pangaea.790791
title: (Appendix C) Geochemistry of pyroxenes from DSDP Leg 92 holes

description: For multiple analyses of a single sample the analysis numbers begin with 1 for the first analysis of any sample and progress to the right.
DOI: 10.1594/pangaea.761373
title: (Table 3) Aeolian component of North Pacific pelagic sediments

description: Isolation and analysis of the eolian component of late Cenozoic pelagic sediments from the North Pacific provides direct information concerning changes in atmospheric circulation. A 50% increase in intensity of both the prevailing westerlies and the tradewinds coincides with increasing pole-to-equator temperature gradients resulting from the onset of northern hemisphere glaciation. At the same time, the mass flux of dust from continents to the North Pacific increased by a factor of 4.5, apparently reflecting significantly increased continental aridity associated with the late Cenozoic glacial ages.
description: Supplement to: Rea, David K; Janecek, Thomas R (1982): Late Cenozoic changes in atmospheric circulation deduced from North Pacific eolian sediments. Marine Geology, 49(1-2), 149-167
DOI: 10.1594/pangaea.745368
title: (Table 7) Analyses of chaleopyrite of ODP Hole 106-649B
DOI: 10.6084/m9.figshare.24547054
title: Additional file 2 of Causal effect between gut microbiota and pancreatic cancer: a two-sample Mendelian randomization study

description: Supplementary Material 2
DOI: 10.6084/m9.figshare.24547054.v1
title: Additional file 2 of Causal effect between gut microbiota and pancreatic cancer: a two-sample Mendelian randomization study

description: Supplementary Material 2
DOI: 10.1594/pangaea.743319
title: (Table 19) Chemical composition of Fe-Mn crusts from the Bouvet Triple Junction area
DOI: 10.1594/pangaea.745282
title: (Table 1) Modal analyses of selected samples of ODP Hole 109-670A
DOI: 10.1594/pangaea.895913
title: Photographs of copepod species from net samples taken during the METEOR cruise M42/3

description: Photographs of copepod species were taken from net samples of the METEOR cruise M42/3 to the Great Meteor Bank. The specimens were identified from formalin preserved samples which is noted in the metadata. Photographs were taken through the ocular of the stereo microscope. No scale is provided, but a link to the respective WoRMS species page where sizes for adults can be found. If available a link to a corresponding dataset on species abundances during the cruises is provided.
DOI: 10.1594/pangaea.691364
title: Mesozooplankton average mass during Mikhail Lomonosov cruise ML24, Part I

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.125 mm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300, 300-500 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.733367
title: Documentation of sediment core MSM12/655-2
DOI: 10.1594/pangaea.744247
title: Physical oceanography during G. O. Sars cruise GS72/3 to the North Sea
DOI: 10.1594/pangaea.733917
title: (Table 2) 226Ra and 210Pb activity ratios of sediment core AII76-18
DOI: 10.1594/pangaea.730180
title: (Table 1) Nd and Sr isotopic compositions and isotope dilution trace element concentrations of sediment core HU91-045-052

description: Isotope dilution concentration determinations are accurate to approx. 1% for Rb and Sr, and 0.5% for Sm and Nd. Total procedural blanks averaged apporx. 1 ng for Sr and 100 pg for Nd, during the study period. Measured 87Sr/86Sr ratios were analyzed using four-collector static mode measurements. Thirty measurements of SRM-987 during the study period yielded mean 87Sr/86Sr=0.71032±2. Measured 143Nd/144Nd normalized to 146Nd/144Nd=0.7219. Analyses were dynamic mode, three-collector measurements. Thirty three measurements of the La Jolla Nd standard during the study period yielded a mean 143Nd/144Nd=0.511838±8 (2sigma mean). e-Nd values are calculated using a present-day 143Nd/144Nd (CHUR)=0.512638. Size fraction &lt;63 µm.
DOI: 10.1594/pangaea.679410
title: Physical oceanography at CTD station CE0506_59
DOI: 10.1594/pangaea.774770
title: Kaolinite/chlorite ratios measured on sediment core PS2498-1