cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.810101
title: (Table 1) Non-arboreal and arboreal pollen spectra at DSDP Holes 75-532 and 75-530A

description: Some samples from DSDP Holes 530A and 532 were analyzed for their fossil pollen content. The sites are located in the southeastern corner of the Angola Basin, about 200 km west of the present coastline.Fossil pollen assemblages of Holocene to Miocene age were compared with present-day pollen deposition in the arid Namib sand sea. The strong resemblance of all the pollen spectra indicates that very arid conditions existed in the coastal region of Namibia in Quaternary and Pliocene times. These data are in agreement with the late Miocene origin of the coastal aridity and with the conception that upwelling of cold water was responsible for these desert conditions.
description: Supplement to: van Zinderen Bakker, Eduard M (1984): Palynological evidence for late Cenozoic arid conditions along the Namibia Coast from Holes 532 and 530A, Leg 75, Deep Sea Drilling Project. In: Hay, WW; Sibuet, J-C; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 75, 763-768
DOI: 10.6084/m9.figshare.24628191
title: Additional file 2 of Genome-wide association study exploring the genetic architecture of eggshell speckles in laying hens

description: Supplementary Table S3. Gene Ontology enrichment analysis of candidate genes
DOI: 10.6084/m9.figshare.24628191.v1
title: Additional file 2 of Genome-wide association study exploring the genetic architecture of eggshell speckles in laying hens

description: Supplementary Table S3. Gene Ontology enrichment analysis of candidate genes
DOI: 10.6084/m9.figshare.26643994
title: Additional file 3 of Genome-wide association study exploring the genetic architecture of eggshell speckles in laying hens

description: Supplementary Table S2. Details of candidate SNPs associated with eggshell speckles
DOI: 10.6084/m9.figshare.26643994.v1
title: Additional file 3 of Genome-wide association study exploring the genetic architecture of eggshell speckles in laying hens

description: Supplementary Table S2. Details of candidate SNPs associated with eggshell speckles
DOI: 10.6084/m9.figshare.26643997
title: Additional file 4 of Genome-wide association study exploring the genetic architecture of eggshell speckles in laying hens

description: Supplementary Table S4. KEGG pathways analysis of candidate genes
DOI: 10.6084/m9.figshare.26643997.v1
title: Additional file 4 of Genome-wide association study exploring the genetic architecture of eggshell speckles in laying hens

description: Supplementary Table S4. KEGG pathways analysis of candidate genes
DOI: 10.1594/pangaea.810382
title: (Appendix D) Isotopic analyses of planktonic foraminifers at DSDP Leg 74 Holes

description: Sediment depth is given in mbsf. Ages are estimated as described in Shackleton et al. 1984 (doi:10.2973/dsdp.proc.74.117.1984).
DOI: 10.6084/m9.figshare.26628949
title: Additional file 9 of Spatial transcriptomics reveal basal sex differences in supraoptic nucleus gene expression of adult rats related to cell signaling and ribosomal pathways

description: Additional file 9. Spreadsheet 7. Compiled GO Terms/Pathway Results for DESeq2 Females vs. Males.
DOI: 10.1594/pangaea.401664
title: Water temperature and current velocity from surface drifter SVP_18828
DOI: 10.1594/pangaea.401628
title: Water temperature and current velocity from surface drifter SVP_18780
DOI: 10.1594/pangaea.401671
title: Water temperature and current velocity from surface drifter SVP_18836
DOI: 10.1594/pangaea.401629
title: Water temperature and current velocity from surface drifter SVP_18783
DOI: 10.1594/pangaea.401634
title: Water temperature and current velocity from surface drifter SVP_18790
DOI: 10.1594/pangaea.56964
title: Physical properties of sediment core PS56/213-2
DOI: 10.1594/pangaea.401644
title: Water temperature and current velocity from surface drifter SVP_18804
DOI: 10.1594/pangaea.401714
title: Water temperature and current velocity from surface drifter SVP_18911
DOI: 10.1594/pangaea.401655
title: Water temperature and current velocity from surface drifter SVP_18818
DOI: 10.1594/pangaea.401676
title: Water temperature and current velocity from surface drifter SVP_18843
DOI: 10.1594/pangaea.401701
title: Water temperature and current velocity from surface drifter SVP_18872
DOI: 10.1594/pangaea.401659
title: Water temperature and current velocity from surface drifter SVP_18822
DOI: 10.1594/pangaea.401663
title: Water temperature and current velocity from surface drifter SVP_18827
DOI: 10.6084/m9.figshare.24628192
title: Additional file 2 of Heterogeneity of outcomes in randomized controlled trials on implant prosthodontic therapy is hindering comparative effectiveness research: meta-research study

description: Supplementary Material 2: List of included systematic reviews and randomized controlled trials
DOI: 10.6084/m9.figshare.24628192.v1
title: Additional file 2 of Heterogeneity of outcomes in randomized controlled trials on implant prosthodontic therapy is hindering comparative effectiveness research: meta-research study

description: Supplementary Material 2: List of included systematic reviews and randomized controlled trials
DOI: 10.1594/pangaea.401650
title: Water temperature and current velocity from surface drifter SVP_18811
DOI: 10.1594/pangaea.401668
title: Water temperature and current velocity from surface drifter SVP_18832
DOI: 10.6084/m9.figshare.26644012
title: Additional file 4 of Heterogeneity of outcomes in randomized controlled trials on implant prosthodontic therapy is hindering comparative effectiveness research: meta-research study

description: Supplementary Material 4: Raw data extractions
DOI: 10.6084/m9.figshare.26644012.v1
title: Additional file 4 of Heterogeneity of outcomes in randomized controlled trials on implant prosthodontic therapy is hindering comparative effectiveness research: meta-research study

description: Supplementary Material 4: Raw data extractions
DOI: 10.1594/pangaea.401651
title: Water temperature and current velocity from surface drifter SVP_18812
DOI: 10.1594/pangaea.401654
title: Water temperature and current velocity from surface drifter SVP_18817
DOI: 10.1594/pangaea.401589
title: Water temperature and current velocity from surface drifter SVP_18693
DOI: 10.1594/pangaea.665822
title: Oceanography at CTD/bottle station IFREMER_2648
DOI: 10.1594/pangaea.401497
title: Water temperature and current velocity from surface drifter SVP_17360
DOI: 10.1594/pangaea.401509
title: Water temperature and current velocity from surface drifter SVP_17454
DOI: 10.1594/pangaea.401486
title: Water temperature and current velocity from surface drifter SVP_17296
DOI: 10.1594/pangaea.401444
title: Water temperature and current velocity from surface drifter SVP_17017
DOI: 10.1594/pangaea.401477
title: Water temperature and current velocity from surface drifter SVP_17281
DOI: 10.1594/pangaea.322205
title: Water temperature real-time profiles from cruise 6222998 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.708769
title: Radiosonde PS71/28788 during POLARSTERN cruise ANT-XXIV/4 on 2008-05-16 11:00h

description: Height of tropopause 10570 m, precipitable water content 1.9675 cm
DOI: 10.1594/pangaea.401415
title: Water temperature and current velocity from surface drifter SVP_16193
DOI: 10.1594/pangaea.708689
title: Mineralogy, isotopic composition of oxygen, hydrogen and carbon, and oxygen isotopic temperature of deep-sea silica and coexisting carbonates (Table 1)

description: Water extracted from opal-CT ("porcellanite", "cristobalite"), granular microcrystalline quartz (chert), and pure fibrous quartz (chalcedony) in cherts from the JOIDES Deep Sea Drilling Project is 56‰ to 87‰ depleted in deuterium relative to the water in which the silica formed. This large fractionation is similar in magnitude and sign to that observed for hydroxyl in clay minerals and suggests that water extracted from these forms of silica has been derived from hydroxyl groups within the silica. Delta18O-values for opal-CT at sites 61, 64, 70B and 149 vary from 34.3‰ to 37.2‰ and show no direct correlation with depth of burial. Granular microcrystaUine quartz in these cores is 0.5 ‰ depleted in 18O relative to coexisting opal-CT at sediment depths of 100 m and the depletion increases to 2‰ for sediments buried below 384 m. These relationships suggest that opal-CT forms before significant burial while granular microcrystalline quartz forms during deeper burial at warmer temperatures. The temperature at which opal-CT forms is thus probably approximately equal to the temperature of the overlying bottom water. Isotopic temperatures deduced for opal-CT formation are preliminary and very approximate, but yield Eocene deep-water temperatures of 5-13°C, and 6°C for the upper Cretaceous sample.Pure euhedral quartz crystals lining a cavity in opal-CT at 388 m in core 8-70B-4-CC have a ~delta18O value of +29.8‰ and probably formed near maximum burial. The isotopic temperature is approximately 32 ° C.
description: Supplement to: Knauth, L Paul; Epstein, Samuel (1975): Hydrogen and oxygen isotope ratios in silica from the Joides Deep Sea Drilling Project. Earth and Planetary Science Letters, 25(1), 1-10
DOI: 10.1594/pangaea.700964
title: (Table 1) Age, thickness of sedimentary cover, depth into volcanic basement, calcite content, and carbon and oxygen isotope data of glassy and crystalline samples from the Atlantic Ocean and the Lau Basin

description: Textural and DNA studies of pillow lavas in DSDP/ODP cores from the Atlantic Ocean, the Lau Basin and the Costa Rica Rift indicate that microbes had a significant role in the alteration of basaltic glasses. Carbon isotopes (d13C) in carbonates from glassy and crystalline basalts from these locations also show differences that may relate to microbial activity during alteration. The generally low d13C values (&lt; -7 per mil) in the basaltic glass of a high proportion of samples from the Atlantic, and most of the Costa Rica Rift material were attributed to alteration influenced by Bacteria and oxidation of organic matter. Positive d13C values of some samples from the Atlantic suggest lithotrophic utilization of CO2, in which methanogenic Archaea produced CH4 from H2 and CO2. This may result from higher abiotic production of H2 in the slow-spreading, fault-dominated Atlantic crust, due to more extensive serpentinization than at the intermediate-spreading Costa Rica Rift.
description: Supplement to: Furnes, Harald; Muehlenbachs, Karlis; Torsvik, Terje; Thorseth, Ingunn H; Tumyr, Ole (2001): Microbial fractionation of carbon isotopes in altered basaltic glass from the Atlantic Ocean, Lau Basin and Costa Rica Rift. Chemical Geology, 173(4), 313-330
DOI: 10.1594/pangaea.415874
title: Granulometry of surface sediments from the Panama Basin (Table 2, 3)

description: Panama Basin sediment surface coarse fractions are dominantly composed of planktonic foraminiferal remains. Textural studies of these coarse fractions by means of a large diameter settling tube system reveal characteristics grain size spectra with important modes at 2.0-2.25 phi, 2.3-2.45 phi, 2.5-2.75 phi, 3.0-33 phi, and 3.4-3.75 phi. The coarser modes consist of large Globoquadrina dutertrei and Globorotalia menardii shells, the finer ones of small planktonic foraminiferal species and of shell fragments of the larger species. Analyses of samples from the Carnegie Gap provide sufficient information such that the extent of the high energy environment close to the sill depth can be mapped; the textural analyses also seem to indicate south and northward flowing components of the bottom currents which transport particle assemblages with distinct textural characteristics. The samples bear evidence for large scale removal of calcareous fines from the crest of structural highs; the fines are then dumped on the flanks of these elevations.
description: Supplement to: Thiede, Jörn (1977): Textural variations of calcareous coarse fractions in the Panama Basin (Eastern Equatorial Pacific Ocean). In: Andersen, N.R. & Malahoff, A. (eds.): The fate of fossil fuel CO2 in the Oceans. Plenum Publishing Corporation, New York, 673-692
DOI: 10.1594/pangaea.804401
title: (Table 1) Calcium carbonate abundance in ODP Leg 164 sites

description: Diffuse reflectance spectra measured during shipboard core description with a hand-held Minolta spectrophotometer are reliable data for interpreting sediment composition. Factor analysis of these spectra indicates that only Glad Cling WrapTM, a polyethylene food wrap, should be used to cover wet cores during measurement because it introduces substantially less noise into the spectra than other brands of plastic food wrap. This validates our previous recommendation that only Glad Cling WrapTM should be used to cover wet core surfaces before spectral analysis on board ship. Factor analysis also indicates that the red end of the spectrum was a little noisy; however, it is unclear if this noise was produced by the Glad Cling WrapTM, by the Minolta instrument, or by the sediment being analyzed when wet (water tends to affect the red end of the spectrum more than the violet). Comparison of spectra taken directly from wet cores on board ship with the Minolta CM-2002 to those taken from dried, prepared samples with our shore-based Perkin-Elmer Lambda 6 spectrophotometer indicates that water mutes the spectral signal. Although factor analysis of the Perkin-Elmer data produced five factors, four of those factors are the same as the factors extracted from the wet core data with the Minolta. This suggests that the water content in the wet cores was not high enough to seriously hinder interpretation of sediment composition. These four common factors are interpreted as carbonate, chlorite or glauconite, organic matter, and iron oxides (probably a mixture of hematite and goethite). The presence of hematite can be attributed to hematite-rich sediment derived from the Canadian Maritime provinces, which has been transported southward by the Western Boundary Undercurrent (WBUC) along North American continental margin. Based on the distribution of hematite down the Leg 164 holes, the WBUC apparently has washed over the Leg 164 sites on the crest of the Blake Ridge only during the Holocene and very latest Pleistocene.
description: Supplement to: Balsam, William L; Damuth, John E (2000): Further investigations of shipboard vs. shore-based spectral data: implications for interpreting Leg 164 sediment composition. In: Paull, CK; Matsumoto, R; Wallace, PJ; Dillon, WP (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 164, 1-12
DOI: 10.1594/pangaea.401608
title: Water temperature and current velocity from surface drifter SVP_18751
DOI: 10.1594/pangaea.785251
title: (Table 1) Results of consolidaten tests for ODP Hole 131-808C and DSDP Hole 87-582 samples

description: Uniaxial reconsolidation tests were conducted on samples from four whole-round cores of similar hemipelagic silty mudstones from the Shikoku Basin sequence recovered at DSDP Site 582 and ODP Site 808. Two cores from Site 808 were from below the d?collement, in the prism toe, and two from Site 582 were from the undeformed trench wedge. The objectives of testing included the estimation of maximum past consolidation stress, the in-situ stress, the exploration of relationships between physical properties and mechanical state of the naturally consolidated mudstones, and comparison of the behavior of these natural sediments with similar but experimentally consolidated mudstone. Testing also determined the effect of pressure between laboratory (1 bar) and in-situ conditions on seismic velocity and on porosity.On the basis of their yield stresses (sigma c'), samples from Site 582 were overconsolidated, whereas those from Site 808 were highly underconsolidated. The apparent overconsolidation at Site 582 is attributed to incipient cementation, which contributes strength and stiffness to the sediment. Porosity in these samples was much higher than that in the experimentally consolidated analog at the same sigma v', which probably reflects higher than hydrostatic pore pressure. However, the effect of excess pore pressure on sigma c' is masked by that of cementation.In part, the underconsolidation at Site 808 is thought to reflect inhibited drainage, primarily occurring as these sediments were subducted beneath the tip of the décollement. The extreme apparent underconsolidation of the sample closest to the décollement is attributed to a reduction of sigma c' caused by destruction of cementation, possibly by isotropic stress pulses of high pore-fluid pressure.The enhanced cementation at Site 582 relative to that at Site 808, which behaves similarly to the uncemented, experimentally consolidated mudstone, results in much higher constrained moduli and higher seismic velocities at equivalent porosities. This demonstrates that velocity-porosity relationships are strongly influenced by very subtle differences in sediment properties. Seismic velocities increased between 5% and 10% between laboratory and in-situ pressures. Most of this increase reflects crackclosing at low pressure. Porosity rebound at both sites was from &lt;1%-2%, far less than for the experimentally consolidated sediment or than was predicted from published values for mudstones.
description: Supplement to: Karig, Daniel E (1993): Reconsolidation tests and sonic velocity measurements of clay-rich sediments from the Nankai Trough. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 247-260
DOI: 10.1594/pangaea.401609
title: Water temperature and current velocity from surface drifter SVP_18752
DOI: 10.1594/pangaea.401610
title: Water temperature and current velocity from surface drifter SVP_18753
DOI: 10.1594/pangaea.401557
title: Water temperature and current velocity from surface drifter SVP_18311
DOI: 10.1594/pangaea.401402
title: Water temperature and current velocity from surface drifter SVP_15989
DOI: 10.6084/m9.figshare.24628079
title: Additional file 1 of Genome-wide identification, expression analysis, and functional study of the bZIP transcription factor family and its response to hormone treatments in pea (Pisum sativum L.)

description: Additional file 1: Supplementary Table 1. List of the 87 PsbZIP genes identified in this study.
DOI: 10.6084/m9.figshare.24628079.v1
title: Additional file 1 of Genome-wide identification, expression analysis, and functional study of the bZIP transcription factor family and its response to hormone treatments in pea (Pisum sativum L.)

description: Additional file 1: Supplementary Table 1. List of the 87 PsbZIP genes identified in this study.
DOI: 10.1594/pangaea.401309
title: Water temperature and current velocity from surface drifter SVP_12975
DOI: 10.1594/pangaea.401528
title: Water temperature and current velocity from surface drifter SVP_17596
DOI: 10.6084/m9.figshare.24628195
title: Additional file 2 of Genome-wide identification, expression analysis, and functional study of the bZIP transcription factor family and its response to hormone treatments in pea (Pisum sativum L.)

description: Additional file 2: Supplementary Table 2. Analysis and distribution of conserved motifs in other plants bZIP proteins.
DOI: 10.6084/m9.figshare.24628195.v1
title: Additional file 2 of Genome-wide identification, expression analysis, and functional study of the bZIP transcription factor family and its response to hormone treatments in pea (Pisum sativum L.)

description: Additional file 2: Supplementary Table 2. Analysis and distribution of conserved motifs in other plants bZIP proteins.
DOI: 10.6084/m9.figshare.26644060
title: Additional file 3 of Genome-wide identification, expression analysis, and functional study of the bZIP transcription factor family and its response to hormone treatments in pea (Pisum sativum L.)

description: Additional file 3: Supplementary Table 3. The tandem duplication events of PsbZIP  genes.
DOI: 10.6084/m9.figshare.26644060.v1
title: Additional file 3 of Genome-wide identification, expression analysis, and functional study of the bZIP transcription factor family and its response to hormone treatments in pea (Pisum sativum L.)

description: Additional file 3: Supplementary Table 3. The tandem duplication events of PsbZIP  genes.
DOI: 10.6084/m9.figshare.26644063
title: Additional file 4 of Genome-wide identification, expression analysis, and functional study of the bZIP transcription factor family and its response to hormone treatments in pea (Pisum sativum L.)

description: Additional file 4: Supplementary Table 4. The 11 pairs of segmental duplicates in  Pisum sativum bZIP genes.
DOI: 10.6084/m9.figshare.26644063.v1
title: Additional file 4 of Genome-wide identification, expression analysis, and functional study of the bZIP transcription factor family and its response to hormone treatments in pea (Pisum sativum L.)

description: Additional file 4: Supplementary Table 4. The 11 pairs of segmental duplicates in  Pisum sativum bZIP genes.
DOI: 10.15468/dl.77e5pk
title: Occurrence Download

description: A dataset containing 9 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is one of (Cynometra congensis De Wild.)"
 ]
}

 The dataset includes 9 records from 4 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0070001-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.401229
title: Water temperature and current velocity from surface drifter SVP_11316
DOI: 10.1594/pangaea.401236
title: Water temperature and current velocity from surface drifter SVP_11382
DOI: 10.6084/m9.figshare.26644066
title: Additional file 5 of Genome-wide identification, expression analysis, and functional study of the bZIP transcription factor family and its response to hormone treatments in pea (Pisum sativum L.)

description: Additional file 5: Supplementary Table 5. One-to-one orthologous relationships between  Pisum sativum and Solanum lycopersicum.
DOI: 10.14457/tu.the.2023.1088
title: การพัฒนาระบบบริหารจัดการผู้มาติดต่ออาคารศูนย์คอมพิวเตอร์

description: รายงานการค้นคว้าอิสระนี้เป็นการพัฒนาแอปพลิเคชันสำหรับศูนย์คอมพิวเตอร์หลักของธนาคารอาคารสงเคราะห์ ซึ่งพัฒนาขึ้นเพื่อบริหารจัดการการเข้าออกอาคาร ข้อมูลการขอเข้าห้องคอมพิวเตอร์และห้องเครือข่าย ข้อมูลการขอเข้าใช้งานห้องประชุมเสมือนจริง โดยผู้ขอใช้งานสามารถสร้างคำขอด้วยตนเองได้ อีกทั้งทีมผู้ดูแลสามารถควบคุมและติดตามการเข้าออกอาคารรวมถึงจัดเก็บข้อมูลในรูปแบบดิจิทัลเพื่อให้ง่ายต่อการค้นหาและการนำมาใช้ประโยชน์ต่อไปในอนาคต ตอบโจทย์การตรวจสอบการเข้าออกอาคารจากหน่วยงานภายนอกและหน่วยงานภายในได้ ซึ่งระบบนี้ทำงานในรูปแบบโมบายแอปพลิเคชันสามารถเข้าถึงได้ทุกที่ทุกเวลา เหมาะสมกับความต้องการใช้งานของผู้ขอและผู้อนุมัติที่ไม่ได้อยู่หน้าคอมพิวเตอร์ตลอดเวลา การพัฒนาแอปพลิเคชันและออกแบบระบบ ผู้พัฒนาใช้สถาปัตยกรรมแบบโมบายแอปพลิเคชัน (Mobile Application) มีการวางแผนการพัฒนาด้วยแนวคิดการคิดวิเคราะห์และออกแบบระบบเชิงวัตถุ (Object-Oriented Analysis and Design) ซึ่งเป็นวิธีการที่ช่วยให้ระบบมีความยืดหยุ่น ง่ายต่อการแก้ไขและพัฒนาต่อยอด อีกทั้งใช้ภาษาดาร์ท (Dart) ภายใต้กูเกิลฟลัตเตอร์ (Google Flutter) ซึ่งเป็นกรอบการพัฒนาข้ามแพลตฟอร์มที่สามารถพัฒนาแอปพลิเคชันที่ใช้งานได้ทั้งในระบบไอโอเอส (IOS) และ แอนดรอยด์ (Android) โดยใช้บริการกูเกิลไฟร์เบส (Google Firebase) ในการจัดการฐานข้อมูลของระบบ