cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.266637
title: X-ray fluorescence data (calcium and iron) of ODP Hole 189-1172D
DOI: 10.1594/pangaea.57062
title: Susceptibility, density, iron and calcium of ODP Hole 165-999B
DOI: 10.1594/pangaea.358949
title: Stable isotopes measured on foraminifera from the 120 kyr time slice reconstruction in sediment core V27-86
DOI: 10.1594/pangaea.97027
title: Sedimentation rates of Hole 2-11

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.81213
title: X-ray fluorescence data of ODP Hole 175-1075A
DOI: 10.1594/pangaea.97065
title: Sedimentation rates of Hole 43-385

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.97002
title: Sedimentation rates of Hole 11-107

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.198839
title: (Table T2) Electron microprobe analyses of iron concentrations within blocky dolomite, ODP Hole 175-1082A

description: Electron microprobe analysis of zoned dolomite was not possible because of its small crystal size (&lt;12 µm) and disseminated nature.
DOI: 10.1594/pangaea.407508
title: Stable isotopes of sediment core C1960.201
DOI: 10.1594/pangaea.407529
title: Stable isotopes of sediment core BA84-02PC
DOI: 10.1594/pangaea.358922
title: Stable isotopes measured on foraminifera from the 120 kyr time slice reconstruction in sediment core RC11-120
DOI: 10.1594/pangaea.407574
title: Stable isotopes of sediment core KC82-41
DOI: 10.1594/pangaea.97001
title: Sedimentation rates of Hole 11-106

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.97010
title: Sedimentation rates of Hole 12-115

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.52268
title: (Table 2) Stable isotope ratios of Globigerina bulloides from DSDP Hole 81-552A
DOI: 10.1594/pangaea.97061
title: Sedimentation rates of Hole 41-370

description: compiled and calculated from various DSDP data sources
DOI: 10.1594/pangaea.81649
title: Stable oxygen and carbon isotope ratios of planktonic foraminifera from sediment core GeoB3104-1
DOI: 10.1594/pangaea.407936
title: Hydrochemistry measured on water bottle samples of third Gironde cruise during BIOGEST
DOI: 10.1594/pangaea.267744
title: Stable isotope ratio of benthic foraminifera from Hole 14-141
DOI: 10.1594/pangaea.186149
title: Stable isotope analysis on planktic foraminifera in sediment core CH119-16PG
DOI: 10.1594/pangaea.407873
title: Stable isotopes of sediment core 75KS19

description: sieve larger than 63
DOI: 10.1594/pangaea.66316
title: Stable isotope data of sediment core GEOFAR KF09
DOI: 10.1594/pangaea.407875
title: Stable isotopes of sediment core 75KS26

description: sieve larger than 63
DOI: 10.1594/pangaea.407513
title: Stable isotopes of sediment core BA82-15PC
DOI: 10.1594/pangaea.228740
title: Stable isotopes of benthic foraminifera from Site 122-761

description: Stable isotopes were measured on Cibicidoides mundulus, and Planulina wuellerstorfi where C. mundulus was absent or rare
DOI: 10.1594/pangaea.267745
title: Stable isotope ratio of benthic foraminifera from Hole 41-366
DOI: 10.1594/pangaea.51479
title: Adjusted stable isotope ratios of Cibicidoides wuellerstorfi and Globigerinoides sacculifer from ODP Hole 130-806B on the Ontong Java Plateau
DOI: 10.1594/pangaea.407933
title: Hydrochemistry measured on water bottle samples of first Scheldt cruise during BIOGEST
DOI: 10.1594/pangaea.106779
title: Stable isotope analysis on sediment core V30-40
DOI: 10.1594/pangaea.56368
title: (Table 1) Stable isotope ratios of foraminifera from sediment core W8402A-14

description: In the publication, d13C and d18O were erroneously exchanged. This is the corrected version.
DOI: 10.1594/pangaea.56805
title: Pollen profile from section Luederholz-2 in northern Germany
DOI: 10.1594/pangaea.60016
title: Stable isotopes on sediment core OK92_2185
DOI: 10.1594/pangaea.56808
title: Pollen profile from section Luttersee-2 in northern Germany
DOI: 10.1594/pangaea.124324
title: Stable isotopes measured on Haynesina orbiculare of sediment core BP01-83/02
DOI: 10.1594/pangaea.124309
title: Stable isotopes of Elphidium bartletti of sediment core BP00-07/05
DOI: 10.1594/pangaea.77491
title: Stable isotope on G. ruber w of sediment core MD77-203
DOI: 10.1594/pangaea.94930
title: Stable isotopes on Cibicidoides subhaidingerii alpha from ODP Hole 182-1129C
DOI: 10.1594/pangaea.407932
title: Hydrochemistry measured on water bottle samples of fourth Scheldt cruise during BIOGEST
DOI: 10.1594/pangaea.52211
title: Stable isotopes of sediment core V19-30 (specmap2.007)
DOI: 10.1594/pangaea.407930
title: Hydrochemistry measured on water bottle samples of third Scheldt cruise during BIOGEST
DOI: 10.1594/pangaea.142634
title: Pollen profile from swamp at Rappershausen site 2, Grabfeld

description: Pollen zones after Firbas Xa-Xb; profile from peat of a Carex elata-bult (40 cm)
DOI: 10.1594/pangaea.94936
title: Stable isotopes measured on Planulina wuellerstorfi from ODP Hole 182-1131B
DOI: 10.1594/pangaea.124316
title: Stable isotopes measured on Elphidium excavatum forma clavata of sediment core BP01-62/06
DOI: 10.1594/pangaea.407929
title: Hydrochemistry measured on water bottle samples of first Sado cruise during BIOGEST
DOI: 10.1594/pangaea.407927
title: Hydrochemistry measured on water bottle samples of fourth Rhine cruise during BIOGEST
DOI: 10.1594/pangaea.124953
title: Barium concentration in pore water of sediment core TT013_5S_B

description: The 0.0 depth interval is defined by the PI as bottom water.
DOI: 10.1594/pangaea.407928
title: Hydrochemistry measured on water bottle samples of first Rhine cruise during BIOGEST
DOI: 10.1594/pangaea.407925
title: Hydrochemistry measured on water bottle samples of third Rhine cruise during BIOGEST
DOI: 10.1594/pangaea.407921
title: Hydrochemistry measured on water bottle samples of second Gironde cruise during BIOGEST
DOI: 10.1594/pangaea.407918
title: Hydrochemistry measured on water bottle samples of first Elbe cruise during BIOGEST
DOI: 10.1594/pangaea.407922
title: Hydrochemistry measured on water bottle samples of fourth Gironde cruise during BIOGEST
DOI: 10.1594/pangaea.407919
title: Hydrochemistry measured on water bottle samples of first Ems cruise during BIOGEST
DOI: 10.1594/pangaea.266985
title: Chemical composition and stable sulfur isotopes in sediment core KOT97-3GC
DOI: 10.1594/pangaea.52484
title: (Table 8b) Stable isotope ratios of foraminifera in sediment core MD84-551
DOI: 10.1594/pangaea.266992
title: Sulphate concentration in sediment core KOT97-8MUC
DOI: 10.1594/pangaea.407869
title: Facies description of sediment core Sula12_60m
DOI: 10.1594/pangaea.407870
title: Facies description of sediment core Sula21
DOI: 10.1594/pangaea.407872
title: Stable isotopes of sediment core 3MO67

description: sieve larger than 63
DOI: 10.1594/pangaea.407885
title: Stable isotopes of sediment core MD84-629
DOI: 10.1594/pangaea.81148
title: CaCO3 and nitrogen isotope data of sediment core VNTR01-2PC
DOI: 10.1594/pangaea.81150
title: CaCO3 and nitrogen isotope data of sediment core VNTR01-4PC
DOI: 10.4225/03/588697a27803b
title: Teachers' self-efficacy, goal orientations, and classroom behaviours: an integrated perspective

description: Although student motivation has been a major focus of basic and applied research in educational psychology for a long time, not many studies have been reported on teacher motivation until recently. Researchers highlight the absence of a sound theoretical framework as the main reason for the lack of research in this area. The current study presents an integrated perspective on teacher motivation by incorporating two different constructs from extant theories (teachers’ self-efficacy from social cognitive theory and goal orientations from achievement goal theory) under the overarching framework of expectancy-value theory. The study analyses the influence of teachers’ self-efficacy (efficacies for classroom management, student engagement, and instructional strategies), and goal orientations (mastery, relational, and work-avoidance) on the selected four dimensions (expectation, structure, relatedness, and autonomy support) of their classroom behaviours. A sample of 257 Victorian primary (n = 115), and secondary (n = 132), school teachers responded to the survey on an 11-point response scale (0-100). Data on teachers’ self-efficacy were collected using Teachers’ Sense of Efficacy Scale (Tschannen-Moran & Woolfolk Hoy, 2001); Goal Orientations for Teaching Scale (Butler, 2012) was used to collect data on teachers’ goal orientations. Data on behavioural dimensions were collected using two scales: Teacher Style Scale (Watt & Richardson, 2007b) and Teacher As Social Context Questionnaire (Belmont, Skinner, Wellborn, & Connell, 1988). The analyses of the data included confirmatory factor analysis (AMOS 20), Multivariate analysis of variance (MANOVA), and, simple, multiple, and canonical correlation analyses (SPSS 20). Paired sample t-tests confirmed the significance of changes in teachers’ self-efficacy during the early career stage. Stepwise multiple regression analyses tested the moderation effects, and structural equation modelling (LISREL) was used to develop the model showing the relationships between the dependent and independent variables in the study. Results indicated positive relationships between teachers’ self-efficacy and their classroom behaviours, further emphasising teachers’ self-efficacy as a key predictor of their classroom behaviours. The malleable nature of self-efficacy was also supported by the data. The negative relationship between teachers’ work-avoidance goal orientations and their classroom behaviours, and the positive association of teachers’ mastery and relational goal orientations with their classroom behaviours were evident with the current data. The data supported the development and testing of a valid structural model relating teachers’ self-efficacy, goal orientations, and classroom behaviours underscoring the significance of expectancy-value theoretical framework in teacher motivation research.
DOI: 10.1594/pangaea.407871
title: Facies description of sediment core Sula22
DOI: 10.1594/pangaea.51937
title: Stable isotopes on foraminifera from sediment core V17-178
DOI: 10.1594/pangaea.319929
title: Age and foraminifera isotopes of Site 151-907
DOI: 10.1594/pangaea.81155
title: CaCO3 and nitrogen isotope data of sediment core VNTR01-9GC
DOI: 10.1594/pangaea.81157
title: CaCO3 and nitrogen isotope data of sediment core YALOC69-071
DOI: 10.1594/pangaea.58250
title: Sedimentology and stable oxygen isotope ratios of Neogloboquadrina pachyderma of core GeoB3375-1
DOI: 10.1594/pangaea.59505
title: (Table 3e) Stable isotope analysis on sediment core BOFS30/3K
DOI: 10.1594/pangaea.52726
title: Stable oxygen isotope record from Globigerina bulloides and sea surface temperature of sediment core BOFS31/1K (Table 1)

description: Two techniques for estimating past variations in sea surface temperature (SST) have been used to investigate climatic change in Biogeochemical Oceanic Flux Study (BOFS) core 31K (19°N, 20°W) from the eastern subtropical Atlantic. High-resolution SST records for the last 28 kyr have been produced using planktonic foraminiferal assemblages, based on the Imbrie-Kipp transfer function technique, and the UK' 37 index derived from abundances of C37 alkenones biosynthesized by prymnesiophyte algae. Modern observations suggest that these indices reflect particular hydrographic conditions in the upper ocean: the UK? 37 index corresponds to the temperature at the time of maximum coccolith productivity, typically late spring-early summer in the study area today, whereas the faunal transfer function is calibrated for seasonal maximum and minimum temperatures. In general, the faunal and biomarker paleotemperature records display comparable SST variations during the last glacial and deglacial, but although the overall trends are similar, differences exist in the magnitude and timing of these temperature changes. Most notably, the faunal T warm and UK' 37 SST estimates diverge by 3°C between 8 ka and 6 ka, and this offset persists through the late Holocene. This difference cannot be adequately explained by uncertainties associated with either the calibration data sets or fluctuating preservation levels. We therefore propose that the deviation in SST estimates is linked to a switch in the seasonal timing of maximum coccolith production from the summer in the glacial ocean to the late spring-early summer in the modern ocean. Our results suggest that a dual approach to SST estimation based on faunal and biomarker proxies can provide a valuable means of evaluating mixed layer and productivity changes associated with the movement of oceanographic frontal zones during the late Quaternary.
description: 2017-09-25: Correction of parameter #4 to SST summer.
description: Supplement to: Chapman, Mark R; Shackleton, Nicholas J; Zhao, Meixun; Eglinton, Geoffrey (1996): Faunal and alkenone reconstructions of subtropical North Atlantic surface hydrography and paleotemperature over the last 28 kyr. Paleoceanography, 11(3), 343-358
DOI: 10.1594/pangaea.69826
title: Age and stable oxygen isotope ratios of Globigerinoides ruber from sediment core M40/4_SL87 in the western Mediterranean Sea
DOI: 10.1594/pangaea.407528
title: Stable isotopes of sediment core 80KB11
DOI: 10.1594/pangaea.267765
title: (Table A2) Stable oxygen isotope ratio of Globigerinoides sacculifer from sediment core ERDC-093P
DOI: 10.1594/pangaea.51481
title: Stable isotopes from ODP Hole 130-806B (Fig. 1)

description: The age of the Brunhes-Matuyama boundary, until recently taken as 730 k.y. in standard time scales for the Quaternary (e.g., Imbrie et al., 1984; Prell et al., 1986, doi:10.1029/PA001i002p00137) and in Ocean Drilling Program results (Kroenke et al., 1991, doi:10.2973/odp.proc.ir.130.1991; Shackleton et al., 1992 doi:10.2973/odp.proc.ir.138.1992) has been revised to between 780 k.y. and 790 k.y., based on both orbital tuning of oxygen isotope data (e.g., Shackleton et al., 1990) and on new 40Ar-39Ar dates on volcanic rocks (e.g., Baksi et al., 1992, doi:10.1126/science.256.5055.356). We apply the revised chronology to an oxygen isotope record for Ontong Java Plateau (ODP Leg 130, western equatorial Pacific). Using this time scale, we find excellent agreement between the record and a template based on orbital forcing. The equation for the template is DeltaICE = IGR - INS a * ICE b * MEM L c [1] where the change in ice-mass is given as the difference between constant ice growth (IGR) and variable amounts of melting. Melting depends on summer insolation at 65°N (INS), the current ice?mass present (ICE), and the average ice?mass (MEM) over a given time interval (L). The memory base L and the exponents are adjusted for best fit. The fit to the relevant portion of the record yields an age of 790±6 k.y. for the Brunhes?Matuyama boundary. The age assignment is robust relative to substantial changes in parameter settings.
description: Supplement to: Berger, Wolfgang H; Bickert, Torsten; Wefer, Gerold; Yasuda, Memorie K (1995): Brunhes-Matuyama boundary: 790 k.y. data consistent with ODP Leg 130 oxygen isotope records based on fit to Milankovitch template. Geophysical Research Letters, 22(12), 1525-1528
DOI: 10.1594/pangaea.106546
title: Stable isotope analysis on sediment core RC11-86

description: Oxygen isotope measurements have been made in foraminifera from over 60 deep-sea sediment cores. Taken together with the oxygen isotope measurements published by Emiliani from Caribbean and Equatorial Atlantic cores, this comprises a unique body of stratigraphic data covering most of the important areas of calcareous sediment over the whole world ocean. The oxygen isotopic composition of foraminifera from cores of Late Pleistocene sediment varies in a similar manner in nearly all areas; the variations reflect changes in the oxygen isotopic composition of the ocean. The oceans are mixed in about 1 ka so that ocean isotopic changes, resulting from fluctuations in the quantity of ice stored on the continents, must have occurred almost synchronously in all regions. Thus the oxygen isotope record provides an excellent means of stratigraphic correlation. Cores accumulated at rates of over about 5 cm/ka provide records of oxygen isotopic composition change that are almost unaffected by post-depositional mixing of the sediment. Thus they preserve a detailed record of the advance and retreat of the ice masses in the northern hemisphere, and provide a unique source of information for the study of ice-sheet dynamics.
DOI: 10.1594/pangaea.407519
title: Stable isotopes of sediment core RC09-191
DOI: 10.1594/pangaea.267763
title: (Table A2) Stable oxygen isotope ratio of Globigerinoides sacculifer from sediment core ERDC-084P
DOI: 10.1594/pangaea.267767
title: (Table A2) Stable oxygen isotope ratio of Globigerinoides sacculifer from sediment core RNDB74
DOI: 10.1594/pangaea.407764
title: Foraminifera distribution of sediment core MD81-BC15

description: counting a min. of 142-294 specimens
DOI: 10.1594/pangaea.67692
title: Color data of sediment core GeoB7207-2
DOI: 10.1594/pangaea.52201
title: Age model and stable isotopes of sediment core RC17-177

description: A careful comparison is made between the most detailed records of sea level over the last glacial cycle, and two high-quality oxygen isotope records. One is a high-resolution benthonic record that contains superb detail but proves to record temperature change as well as ice volume; the other is a planktonic record from the west equatorial Pacific where the temperature effect may be minimal but where high resolution is not available. A combined record is generated which may be a better approximation to ice volume than was previously available.This approach cannot yet be applied to the whole Pleistocene. However, comparison of glacial extremes suggests that glacial extremes of stages 12 and 16 significantly exceeded the last glacial maximum as regards ice volume and hence as regards sea level lowering. Interglacial stages 7, 13, 15, 17 and 19 did not attain Holocene oxygen isotope values; possibly the sea did not reach its present level. It is unlikely that sea level was glacio-eustatically higher than present by more than a few metres during any interglacial of the past 2.5 million years.
description: Supplement to: Shackleton, Nicholas J (1987): Oxygen isotopes, ice volume and sea level. Quaternary Science Reviews, 6(3-4), 183-190
DOI: 10.15468/dl.y98c6d
title: Occurrence Download

description: A dataset containing 1 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((-123.88888 48.55182,-122.32357 48.55182,-122.32357 49.78409,-123.88888 49.78409,-123.88888 48.55182))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Allium paradoxum (M.Bieb.) G.Don"
 ]
}

 The dataset includes 1 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031626-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.407706
title: Density of sediment core OD96_24:6:1
DOI: 10.1594/pangaea.52207
title: Stable isotopes of sediment core ELT49.018-PC (specmap2.006)
DOI: 10.1594/pangaea.93186
title: Physical oceanography at station POS212/3-CTD-856_077
DOI: 10.1594/pangaea.407707
title: Density of sediment core OD96_25:6:1
DOI: 10.1594/pangaea.407687
title: Facies determination of sediment core Nov1
DOI: 10.1594/pangaea.407689
title: Nutrients measured on water bottle samples LOIS-Bottle-175254
DOI: 10.1594/pangaea.407676
title: Facies determination of sediment core Uz1
DOI: 10.1594/pangaea.106548
title: Stable isotope analysis on sediment core RC12-294
DOI: 10.1594/pangaea.56010
title: (Table E1) Accumulation rate, CaCO3, TOC of Site 151-909
DOI: 10.1594/pangaea.139212
title: Grain density in sediment core SO106-251KL
DOI: 10.1594/pangaea.407669
title: Facies determination of sediment core Micha
DOI: 10.1594/pangaea.139213
title: Grain density in sediment core SO106-254KL
DOI: 10.1594/pangaea.407659
title: Facies determination of sediment core Dept1
DOI: 10.1594/pangaea.407666
title: Facies determination of sediment core Ln1
DOI: 10.1594/pangaea.407668
title: Facies determination of sediment core Mam2
DOI: 10.1594/pangaea.103588
title: Carbon and Nitrogen analysis of sediment core Fruela96_B6
DOI: 10.1594/pangaea.407658
title: Facies determination of sediment core Ary1
DOI: 10.1594/pangaea.67690
title: Color data of sediment core GeoB7203-2
DOI: 10.1594/pangaea.52424
title: Sedimentology of ODP Hole 113-693B
DOI: 10.1594/pangaea.59995
title: Oxygen isotope data from snowpit at GISP2 Site 44

description: Data from shallow cores recov. over a 150x150 km grid in central Greenland. Dating of samples based on seasonal variation in oxygen isotope stratigraphy, along with measurements of gross beta activity. Age based on spline interpolation.
DOI: 10.1594/pangaea.327544
title: Time series of upwelling rates in Trujillo, Peru in 1954
DOI: 10.1594/pangaea.74109
title: Gain size distribution of ODP Hole 104-643A
DOI: 10.1594/pangaea.407647
title: Foraminifera abundance of sediment core IN68-7

description: counting a min. of 200 specimens
DOI: 10.1594/pangaea.407639
title: Foraminifera abundance of sediment core BS78-12

description: counting a min. of 200 specimens
DOI: 10.1594/pangaea.407642
title: Foraminifera abundance of sediment core IN68-23
DOI: 10.1594/pangaea.136404
title: Grain size analysis of sediment core IO1277.019-PC
DOI: 10.1594/pangaea.136408
title: Grain size analysis of sediment core IO1277.032-PC
DOI: 10.1594/pangaea.62318
title: PKDB126638

description: Expedition Tibet 1992, data based on diary of B. Frenzel
DOI: 10.1594/pangaea.136412
title: Grain size analysis of sediment core IO1578.007-PC
DOI: 10.1594/pangaea.136415
title: Grain size analysis of sediment core IO1578.041-PC
DOI: 10.1594/pangaea.91228
title: Grain size parameters of sediments of ODP Hole 119-739A
DOI: 10.1594/pangaea.91232
title: Grain size parameters of sediments of ODP Hole 119-743A
DOI: 10.1594/pangaea.407631
title: Foraminifera abundance of sediment core C1960.199

description: counting a min. of 100-1000 specimens
DOI: 10.1594/pangaea.126738
title: XRF results of chemical composition of sediment core PSEE-18
DOI: 10.1594/pangaea.57568
title: Geochemistry of surface sediments from Lake Lama
DOI: 10.1594/pangaea.407625
title: Hydrochemistry and process data measured at EUROTROPH station Scheldt_2
DOI: 10.1594/pangaea.79526
title: Stratigraphic occurrence of selected diatom species from the Miocene at ODP Site 177-1088

description: D (dominant) = &gt;60 % of assemblage; A (abundant) = 30-60 % of assembl.; C (common) = 15-30% of assembl.; F (few) = 3-15 % of assembl.; R(rare) = 0.5-3% of assembl.; T(trace) = sporadically occurrence; X(present) = diatom valves cannot be counted individually.
DOI: 10.1594/pangaea.198760
title: (Table T1) Sample identification, depth, age, and oxygen and carbon isotopic composition of planktic and benthic foraminifers, ODP Hole 175-1087A

description: Timescale calibration after Imbrie et al., (1984), Martinson et al. (1987), and Bassinot et al. (1994). Linear interpolation was applied between adjacent age control-points, assuming a constant sedimentation rate within the time interval.
DOI: 10.1594/pangaea.198840
title: (Table T2) Electron microprobe analyses of iron concentrations within weakly luminescent dolomicrite, ODP Hole 175-1082A

description: Electron microprobe analysis of zoned dolomite was not possible because of its small crystal size (&lt;12 µm) and disseminated nature.
DOI: 10.1594/pangaea.198841
title: (Table T2) Electron microprobe analyses of iron concentrations within blocky dolomite, ODP Hole 175-1084A

description: Electron microprobe analysis of zoned dolomite was not possible because of its small crystal size (&lt;12 µm) and disseminated nature.
DOI: 10.1594/pangaea.407619
title: Foraminifera abundance of sediment core AC85-4

description: counting a min. of 300 specimens