cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.358295
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core RC17-98
DOI: 10.1594/pangaea.51980
title: Distribution of planktic foraminifers of sediment core D117
DOI: 10.1594/pangaea.134130
title: Planktic foraminifera assemblage in sediment core GIK17725-1
DOI: 10.1594/pangaea.51979
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core A180-073
DOI: 10.1594/pangaea.134160
title: Planktic foraminifera assemblage in sediment core GIK23243-2
DOI: 10.1594/pangaea.646255
title: Faunal assemblage of sediment core GS7603-8

description: Fraction 315-400 and &gt;400: G. sacculifer sacculifer and G. sacculifer trilobus are combined.
DOI: 10.1594/pangaea.358292
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core RC13-205
DOI: 10.1594/pangaea.646251
title: Faunal assemblage of sediment core GS7603-12

description: Fraction 315-400 and &gt;400: G. sacculifer sacculifer and G. sacculifer trilobus are combined.
DOI: 10.1594/pangaea.904322
title: Stoichiometric and sterol responses of dinoflagellates to changes in temperature, nutrient supply in the exponential phase

description: We investigated the responses of elemental stoichiometry (POC, PON) and sterol contents (brassicasterol, dinosterol) in three dinoflagellate species (Prorocentrum donghaiense, Prorocentrum minimum and Karenia mikimotoi) to changes in temperatures (15, 20 and 25 °C), N:P supply ratios (molar ratios 10:1, 24:1 and 63:1) in the exponential phase in batch culture experiments.
description: Supplement to: Chen, Mengna; Bi, Rong; Chen, Xi; Ding, Yang; Zhang, Hailong; Li, Li; Zhao, Meixun (2019): Stoichiometric and sterol responses of dinoflagellates to changes in temperature, nutrient supply and growth phase. Algal Research, 42, 101609
DOI: 10.1594/pangaea.846924
title: Relative abundance of planktic foraminifera and calculated SSTs and SST anomaly (0-25.5 ka BP) in sediment core MD99-2284
DOI: 10.1594/pangaea.358309
title: Relative abundance of planktic foraminifera in sediment core RC17-69
DOI: 10.1594/pangaea.134144
title: Planktic foraminifera assemblage in sediment core GIK23256-1
DOI: 10.1594/pangaea.819874
title: Calcareous plankton response to orbital and millennial-scale climate changes from ODP Leg 161-975

description: The paleoenvironmental conditions through MIS 15-9 at the Mediterranean Ocean Drilling Program (ODP) Site 975 were interpreted by high resolution study of calcareous plankton assemblages compared with available d18O and d13C records and high resolution paleoclimate proxies from the Atlantic Ocean. Sea Surface Temperatures (SSTs) have been estimated from planktonic foraminiferal assemblages using the artificial neural networks method. Calcareous plankton varied dominantly on a glacial-interglacial scale as testified by the SST record, foraminiferal diversity, total coccolith abundance and changes in warm-water calcareous nannofossil taxa. A general increase in foraminiferal diversity and of total coccolith abundance is observed during interglacials. Warmest SSTs are reached during MIS 11, while MIS 12 and MIS 10 represent the coldest intervals of the studied record. During MIS 12, one of the most extreme glacials of the last million years, occurrence of Globorotalia inflata and of neogloboquadrinids indicates a shoaling of the interface between Atlantic inflowing and Mediterranean outflowing waters. Among calcareous nannofossils the distribution of Gephyrocapsa margereli-G. muellerae &gt; 4 µm also supports a reduced Atlantic-Mediterranean exchange during MIS 12. Superimposed on glacial-interglacial variability, six short-terms coolings are recognized during MIS 12 and 10, which appear comparable in their distribution and amplitude to the Heinrich - type events documented in the Atlantic Ocean in the same interval. During these H-type events, N. pachyderma (s) and G. margereli-G. muellerae &gt; 4 µm increase as a response to the enhanced inflow of cold Atlantic water into the Mediterranean via the Strait of Gibraltar. Mediterranean surface water hydrography appears to have been most severely affected at Termination V during the H-type event Ht4, possibly as a response to a large volume of Atlantic meltwater inflow via the Strait of Gibraltar and/or to freshwater/terrigenous input deriving from local mountain glaciers. Three additional SST coolings are recorded through MIS 14-16, but these are not well correlated with Heinrich - type events documented in the Atlantic Ocean in the same interval; during these cooling episodes only the subpolar Turborotalita quinqueloba increases. These results highlight the sensitive response of the Mediterranean basin to millennial-scale climate variations related to Northern Hemisphere ice-sheet instability and support the hypothesis that the tight connection between high latitude climate dynamics and Mediterranean sea surface water features can be traced through the Middle Pleistocene.
description: Sediment depth is given in mcd.
description: Supplement to: Girone, Angela; Maiorano, Patrizia; Marino, Maria; Kucera, Michal (2013): Calcareous plankton response to orbital and millennial-scale climate changes across the Middle Pleistocene in the western Mediterranean. Palaeogeography, Palaeoclimatology, Palaeoecology, 392, 105-116
DOI: 10.1594/pangaea.866883
title: Planktonic foraminiferal abundances in sediment core Q585
DOI: 10.1594/pangaea.676909
title: Planktic foraminifera distribution of sediment core GIK17666-2

description: Calendar ages are estimated by interpolation between MIS boundaries from Fretzdorff et al. (2000) and correlation with global ice volume record by Labeyrie et al. (1987) / P/D intergrades encompass specimens that do not satisfy the sensu stricto definitions of neither N. pachyderma (dex) nor N. dutertrei.
DOI: 10.1594/pangaea.134102
title: Planktic foraminifera assemblage in sediment core GIK23065-2
DOI: 10.1594/pangaea.866902
title: Planktonic foraminiferal abundances in sediment core P69
DOI: 10.1594/pangaea.134134
title: Planktic foraminifera assemblage in sediment core GIK17732-1
DOI: 10.1594/pangaea.134156
title: Planktic foraminifera assemblage in sediment core Q208
DOI: 10.1594/pangaea.87440
title: Planktic foraminiferal species counts in GeoB1117-2
DOI: 10.1594/pangaea.807318
title: (Appendix) Planktonic foraminifera abundances in ODP Site 138-847B

description: Sediments from Site 847 in the eastern equatorial Pacific Ocean provide a record of the variability of the equatorial divergence and associated upwelling. We interpret the variation in foraminifer assemblages in the context of regional Oceanographic change. Our record is composed of three time slices selected from the last 0.9 Ma. A Q-mode analysis of foraminifer abundance data results in a four-factor model that was used to quantify the faunal changes and to characterize paleoceanographic variability. The species of foraminifers with high factor scores for each factor suggested a specific set of Oceanographic conditions. The timing of the high loadings for each factor appears to be associated with a particular part of a glacial cycle. Thus, we interpreted our findings in the context of the glacial/interglacial cycle proposed by Imbrie et. al. (1992). This idealized cycle consists of four stages that are defined by characteristic changes in specific elements of the climate system. We evaluated how such changes in the climate system might affect the Oceanographic conditions at Site 847.Our results suggest that upwelling remains a dominant process in both glacial and interglacial stages, but decreases significantly on most deglacials. Subantarctic mode water formation and equatorial upwelling appear to form a linked system that determines the specific characteristics of the water forming a major part of the Equatorial Undercurrent as well as the transport volume of the undercurrent. In conjunction with changes in upwelling at Site 847, this variation in the undercurrent results in changes in mixed layer depth, sea-surface temperature, and oxygen and nutrient levels at the site.
description: DEPTH, sediment is given in mbsf. Time Slice 1 (TSI) covers oxygen isotope stages 1 to 6 (0-0.135 Ma), Time Slice 2 (TS2) covers stages 11 to 14 (0.395-0.572 Ma), and Time Slice 3 (TS3) covers stages 18 to 21 (0.704-0.852 Ma).
description: Supplement to: McKenna, V S; Farrell, John W; Murray, David W; Clemens, Steven C (1995): The foraminifer record at Site 847: Paleoceanographic response to late Pleistocene climate variability. In: Pisias, NG; Mayer, LA; Janecek, TR; Palmer-Julson, A; van Andel, TH (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 138, 695-714
DOI: 10.1594/pangaea.358302
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V28-127
DOI: 10.1594/pangaea.81111
title: Foraminifera and stable isotopes of sediment core PS1754-1
DOI: 10.1594/pangaea.358301
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V27-86
DOI: 10.1594/pangaea.358305
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V28-56
DOI: 10.1594/pangaea.134122
title: Planktic foraminifera assemblage in sediment core GIK17050-1
DOI: 10.1594/pangaea.81114
title: Foraminifera and stable isotopes of sediment core PS2076-3
DOI: 10.1594/pangaea.81113
title: Foraminifera and stable isotopes of sediment core PS2076-1
DOI: 10.1594/pangaea.358294
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core RC13-229
DOI: 10.1594/pangaea.358308
title: Relative abundance of planktic foraminifera in sediment core RC08-39
DOI: 10.1594/pangaea.134146
title: Planktic foraminifera assemblage in sediment core SO42-74KL
DOI: 10.1594/pangaea.56421
title: Percentages of planktonic foraminifera species in sediment core RC24-27
DOI: 10.1594/pangaea.848404
title: Age model of IODP SIte 339-U1387
DOI: 10.15468/dl.t7jcn5
title: Occurrence Download

description: A dataset containing 1258 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Parkinsonia praecox (Ruiz & Pav.) Hawkins)",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 "HasGeospatialIssue is false",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil, Specimen)"
 ]
 }
 }
 ]
}

 The dataset includes 1258 records from 22 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0038672-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.17632/g47z49pk76.1
title: Explosions dataset (L1 Halo orbits)

description: Explosions along orbits of L1 Halo family. The folder includes the initial conditions of the orbits studied and separated mat files for each explosion. In addition, a JSON file is saved including all the information of the explosions in case of computing simulations outside Matlab.
Explosions' files include the state vectors of the fragments for discrete time steps over two years of evolution and classify debris whether fragments escape the system, impact the Earth or the Moon, or continue orbiting throughout the region.
DOI: 10.1594/pangaea.386517
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V30-97
DOI: 10.1594/pangaea.134158
title: Planktic foraminifera assemblage in sediment core SU92-21
DOI: 10.1594/pangaea.386455
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core V27-20
DOI: 10.17632/jnr2z36g77.1
title: Hydrological drought prediction and its influencing factors analysis based on a machine learning model

description: Extreme Gradient Boosting ( XGBoost ) model and Shapley Additive Explanation ( SHAP ) variable importance index in python code. The data is 1 ° * 1 ° grid point related data of Huaihe River Basin.
DOI: 10.1594/pangaea.866879
title: Planktonic foraminiferal abundances in sediment core 90-594
DOI: 10.17632/5yf3c2mk66.1
title: Intelligent Detection of Office Occupancy Based on Hybrid Data Mining

description: This study aims to use hybrid data mining technology to realize office occupancy intelligent detection to improve space utilization, reduce energy consumption, and enhance employee efficiency. Firstly, K-means clustering is carried out on the original data after pre-processing by fusing images, sensors, and behavioral data, and the data is divided into different clusters. Secondly, the Deep Residual Attention Network (DRAN) is utilized to extract the feature from the data of each cluster. Finally, the Weighted Voting-based Extreme Learning Machine (WV-ELM) is employed to classify and detect the data, to realize the occupancy status identification with higher precision. The results show that the proposed model’s accuracy achieves 96.17%, at least an improvement of 6.23%. When iteration times are 100, precision, F1 score, and recall reach 91.30%, 90.96%, and 89.22%, respectively. Moreover, the proposed algorithm outperforms other comparison algorithms on Root Mean Square Error (RMSE), Mean Absolute Error (MAE), and Mean Absolute Percentage Error (MAPE), among which RMSE decreases from 5.83 in 20 epochs to 4.66 in 100 epochs, MAE from 8.46 to 7.08, and MAPE from 10.52 to 8.00. Therefore, the detection system proposed in this study is superior to the existing technology in terms of accuracy, real-time, and robustness, and provides effective technical support for the space management and resource optimization of intelligent buildings.
DOI: 10.1594/pangaea.134128
title: Planktic foraminifera assemblage in sediment core GIK17724-1
DOI: 10.17632/yv5wjymcxn.1
title: Los bioestimulantes mejoran el crecimiento de plantines de una conífera nativa de los Andes (Podocarpus glomeratus) en vivero y campo

description: En esta base de datos compartimos la sobrevivencia y crecimiento de plantines de Podocarpus glomeratus en condiciones de vivero y en condiciones de pastizales degradados de los Andes en Bolivia.
DOI: 10.1594/pangaea.358285
title: Relative abundance of planktic foraminifera in sediment core K11
DOI: 10.1594/pangaea.134092
title: Planktic foraminifera assemblage in sediment core GeoB1113-4
DOI: 10.17632/hyg3f3p6hd.1
title: Influence of whole-body hyperthermia on mRNA expression in PBMCs from ME/CFS patients

description: These data show the measurement of mRNA expression in human PBMCs. The mRNA expression was measured in ME/CFS patients before and after whole-body hyperthermia treatment (1 hour at 39 °C). The following files show the Ct values of mRNA expression of the genes RPLP0, beta-actin, ULK1, Beclin 1, AMPK1α, ATG7, FOXO3, HSPA5, IL-10, MAP1LC3B, SIRT1, SIRT3, TFAM, NDUFS1 and SOD2. The n-fold gene expression after calculation with the 2-ΔΔCt method shows a significant decrease in SIRT3 expression as a result of whole-body hyperthermia. Some other genes show slight but not significant changes.
DOI: 10.1594/pangaea.134118
title: Planktic foraminifera assemblage in sediment core GIK17045-3
DOI: 10.1594/pangaea.866885
title: Planktonic foraminiferal abundances in sediment core S794
DOI: 10.1594/pangaea.134098
title: Planktic foraminifera assemblage in sediment core GIK23055-2
DOI: 10.1594/pangaea.646256
title: Faunal assemblage of sediment core GS7603-9

description: Fraction 315-400 and &gt;400: G. menardii dextral and G. menardii sinistral are combined and G. truncatulinoides dextral and G. truncatulinoides sinistral are combined.
DOI: 10.17632/b6s22s2ny5.1
title: Data for 'Rhizobial variation, more than plant variation, mediates plant symbiotic and fitness responses to herbicide stress'

description: Data associated with the original research article 'Rhizobial variation, more than plant variation, mediates plant symbiotic and fitness responses to herbicide stress', accepted for publication in Ecology. See file 'TFM2020_Data_11-30-23_copy.csv' for raw data and file 'TFM2020_metadata_04-19-24.xlsx' for the accompanying metadata.
DOI: 10.1594/pangaea.134110
title: Planktic foraminifera assemblage in sediment core GIK23071-3
DOI: 10.17632/4kkk45tgdd.1
title: Supplemental files for JAAD research letter

description: Enhancing Nail Width: The Impact of Soft-Tissue Excision on Ingrown Toenails
DOI: 10.17632/vy5z29r5pg.1
title: LC3-II fluorescence intensity in PBMCs from healthy donors and ME/CFS patients (CTRL + whole-body hyperthermia)

description: These data show the antibody-based flow cytometric measurement of the autophagy marker LC3-II in PBMCs. LC3-II levels were measured in ME/CFS patients before and after a session of whole-body hyperthermia (1 h at 39 °C) and in a healthy control group without treatment. The data show a higher LC3-II level in ME/CFS patients compared to healthy donors and a decrease in autophagy due to treatment with wIRA.
DOI: 10.17632/4kkk45tgdd.2
title: Supplemental files for JAAD research letter

description: Enhancing Nail Width: The Impact of Soft-Tissue Excision on Ingrown Toenails
DOI: 10.1594/pangaea.358290
title: Relative abundance of planktic foraminifera in the 120 kyr time slice reconstruction of sediment core RC12-294
DOI: 10.1594/pangaea.746224
title: (Table 6) Relative abundances of the seven species of planktonic foraminifera from ODP Site 108-662

description: Depth, sediment (m) is composite depth (mcd). Full assemblage counts (second value listed) and quick counts with seven species (first value listed) are given; spliced record.
DOI: 10.1594/pangaea.681700
title: Relative abundance of planktonic foraminifera in Pliocene and Pleistocene sediments of DSDP Hole 32-310 from Hess Rise, Central North Pacific (Table II)

description: Late Neogene planktonic foraminifera have been examined at Site 310 in the Central North Pacific and their stratigraphic ranges and frequencies are presented here. Blow's (1969) zonation developed for tropical regions has been applied where applicable. Where tropical index taxa are rare or absent in this temperate region, Globorotalia crassaformis, and the evolutionary bioseries G. conoidea - G. conomiozea and G. puncticulata - G. inflata have been found useful for zonal subdivisions. A correlation between stratigraphic ranges and frequency distributions of these species at Site 310 in the Central North Pacific, and Site 284 in the Southwest Pacific indicates that these species are relatively consistent biostratigraphic markers in temperate regions of both the North and South Pacific Oceans. An informal zonation for temperate latitudes of the Southwest Pacific has been established by Kennett (1973) and a similar zonal subdivision can be made at Site 310. Paleoclimatic/paleoceanographic interpretations based on coiling ratios, percent abundance, and phenotypic variations of Neogloboquadrina pachyderma indicate four major cold events during early, middle, and late Pliocene, and early Pleistocene. Faunal correlations of these events with similar events elsewhere in the Northeast and Southwest Pacific which have been paleomagnetically dated indicate the following approximate ages for these cold events: 4.7 Ma, 3.0 Ma, 2.6-1.8 Ma, and 1.2 Ma. Faunal assemblages have been divided into three groups representing cool, intermediate, and warmer water assemblages. Cool water assemblages are dominated by ~60% N. pachyderma; intermediate temperature faunas are dominated by species of Globigerina and Globigerinita and contain between 20% and 30% N. pachyderma. Warmer water assemblages are dominated by species of Globorotalia and contain &lt;10% N. pachyderma. Frequency oscillations within these groups, in addition to paleotemperature parameters evident in N. pachyderma, afford refined paleoclimatic/paleoceanographic interpretations.
description: Supplement to: Keller, Gerta (1978): Late Neogene biostratigraphy and paleoceanography of DSDP Site 310 Central North Pacific and correlation with the Southwest Pacific. Marine Micropaleontology, 3(2), 97-119
DOI: 10.17632/2w6bxf466y.1
title: High-precision Low-cost Fabrication of Dental Surgical Guides Using Dental Grade Photocurable Resin Through a Hybrid Additive-Subtractive Machine with Reverse Scanning

description: Supplementary information for the manuscript titled 'High-precision Low-cost Fabrication of Dental Surgical Guides Using Dental Grade Photocurable Resin Through a Hybrid Additive-Subtractive Machine with Reverse Scanning'
DOI: 10.1594/pangaea.728968
title: Relative abundances of planktonic foraminifera in ODP Site 121-758 (Table 1)

description: We present a high-resolution (6 k.y. sample interval) record of planktonic foraminifer faunal variations for the past 800 k.y. from ODP Site 758 in the northeastern Indian Ocean. The record is examined within the context of a coarse fraction stratigraphy which is a lithologic index of CaCO3 preservation, and an oxygen isotope stratigraphy which provides a chronostratigraphy and a record of climate change. Variations in the relative abundance of 27 planktonic foraminifer species primarily reflect fluctuations in the intensity of CaCO3 dissolution. CaCO3 dissolution covaries with climate fluctuations at a cyclicity of about 100 k.y. Glacial-aged sediments are generally well preserved, as indicated by faunal and lithologic indices. Interglacial-aged sediments show poorer preservation. The -100-k.y. cycles are superimposed upon the long-term Brunhes Dissolution Cycle. This cycle is characterized by an interval of poor preservation centered between 400 and 550 ka and is bounded by good preservation events at 25 and 750 ka. Ecological factors also control variations in the foraminifer fauna. Changes in ecology are inferred from downcore fluctuations in the relative abundances of foraminifer species that have a similar level of resistance to dissolution. We focus on three species (Neogloboquadrina dutertrei, Pulleniatina obliquiloculata, Globorotalia menardii) with a relatively high resistance to dissolution. The long-term increase in N. dutertrei since at least 800 ka is interpreted as either a gradual decrease in the sea-surface salinity, or an increase in the biogenic productivity of the surface waters. These factors may be controlled by the strength of the monsoon climate. Extremely high abundances of P. obliquiloculata are observed in certain downcore intervals and are interpreted as times when the surface water conditions in the northeast Indian Ocean were similar to those in the modern western tropical Pacific, but not the modern Indian Ocean.
description: Depth, sediment (m) is composite depth (mcd). Ashlayer A between 1.61 to 1.81 mcd samples 121-758A-1H-2,11; 121-758A-1H-2,21; 121-758A-1H-2,31. Ashlayer B at 2.01 mcd sample 121-758A-1H-2,51. Ashlayer C at 8.53 mcd sample 121-758A-2H-1,111. Ashlayer D between 12.23 and 12.33 mcd samples 121-758A-2H-4,31 and 121-758A-2H-4,41.
description: Supplement to: Chen, Min-Te; Farrell, John W (1991): Planktonic foraminifer faunal variations in the northeastern Indian Ocean: a high-resolution record of the past 800,000 years from Site 758. In: Weissel, J; Peirce, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 121, 125-140
DOI: 10.1594/pangaea.646253
title: Faunal assemblage of sediment core GS7603-14

description: Fraction 315-400 and &gt;400: G. sacculifer sacculifer and G. sacculifer trilobus are combined.