cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/3x8s3y
title: An annotated checklist of Myerslopiidae with notes on the distribution and origin of the group (Hemiptera: Cicadomorpha)

description: This dataset contains the digitized treatments in Plazi based on the original journal article Szwedo, Jacek (2004): An annotated checklist of Myerslopiidae with notes on the distribution and origin of the group (Hemiptera: Cicadomorpha). Zootaxa 425 (1): 1-15, DOI: 10.11646/zootaxa.425.1.1, URL: https://biotaxa.org/Zootaxa/article/view/zootaxa.425.1.1
DOI: 10.15468/ct3udu
title: A new species of Nasusina Pearsall from Colorado (Lepidoptera: Geometridae: Eupitheciini)

description: This dataset contains the digitized treatments in Plazi based on the original journal article Ferris, Clifford D. (2004): A new species of Nasusina Pearsall from Colorado (Lepidoptera: Geometridae: Eupitheciini). Zootaxa 467 (1): 1-9, DOI: 10.11646/zootaxa467.1.1, URL: https://biotaxa.org/Zootaxa/article/view/zootaxa467.1.1
DOI: 10.5287/bodleian:0ogqp5bb5
title: luox-2021-0004 deposition
DOI: 10.15468/hu53v7
title: Deep-water Galatheidae (Crustacea: Decapoda: Anomura) from southern and eastern Australia

description: This dataset contains the digitized treatments in Plazi based on the original journal article Ahyong, Shane T., Poore, Gary C. B. (2004): Deep-water Galatheidae (Crustacea: Decapoda: Anomura) from southern and eastern Australia. Zootaxa 472 (1): 1-76, DOI: 10.11646/zootaxa.472.1.1, URL: https://biotaxa.org/Zootaxa/article/view/zootaxa.472.1.1
DOI: 10.3886/e135221
title: Data and Code for: "Stability of Experimental Results: Forecasts and Evidence"

description: This deposit contains code and data for "Stability of Experimental Results: Forecasts and Evidence"<br>Abstract: "How robust are experimental results to changes in design? And can researchers anticipate which changes matter most? We consider a real-effort task with multiple behavioral treatments, and examine the stability along six dimensions: (i) pure replication; (ii) demographics; (iii) geography and culture; (iv) the task; (v) the output measure; (vi) the presence of a consent form. We find near perfect replication of the experimental results, and full stability of the results across demographics, significantly higher than a group of experts expected. The results differ instead across task and output change, mostly because the task change adds noise to the findings."
description: MTurk.
DOI: 10.3886/e135221v1
title: Data and Code for: "Stability of Experimental Results: Forecasts and Evidence"

description: This deposit contains code and data for "Stability of Experimental Results: Forecasts and Evidence"<br>Abstract: "How robust are experimental results to changes in design? And can researchers anticipate which changes matter most? We consider a real-effort task with multiple behavioral treatments, and examine the stability along six dimensions: (i) pure replication; (ii) demographics; (iii) geography and culture; (iv) the task; (v) the output measure; (vi) the presence of a consent form. We find near perfect replication of the experimental results, and full stability of the results across demographics, significantly higher than a group of experts expected. The results differ instead across task and output change, mostly because the task change adds noise to the findings."
description: MTurk.
DOI: 10.15468/jcr5gq
title: Two new species of Opheliidae (Annelida: Polychaeta): Euzonus papillatus sp. n. from a northeastern Brazilian sandy beach and Euzonus mammillatus sp. n. from the continental shelf of southeastern Brazil

description: This dataset contains the digitized treatments in Plazi based on the original journal article Santos, Cinthya S. G., Nonato, Edmundo F., Petersen, Mary E. (2004): Two new species of Opheliidae (Annelida: Polychaeta): Euzonus papillatus sp. n. from a northeastern Brazilian sandy beach and Euzonus mammillatus sp. n. from the continental shelf of southeastern Brazil. Zootaxa 478 (1): 1-12, DOI: 10.11646/zootaxa.478.1.1, URL: https://biotaxa.org/Zootaxa/article/view/zootaxa.478.1.1
DOI: 10.5517/ccdc.csd.cc25f73z
title: CCDC 2008710: Experimental Crystal Structure Determination

description: Related Article: Abdulaziz A. Alanazi, Lukasz Wojtas, Jacob M. Mayers, Jaroslava Miksovska, Randy W. Larsen|2020|Dalton Trans.|49|11668|doi:10.1039/D0DT02050H
DOI: 10.3886/e146342v1
title: Behavioral Risk Factor Surveillance System (BRFSS) Annual Survey Data, 1999-2015

description: In 1984, the Centers for Disease Control and Prevention (CDC) initiated the state-based Behavioral Risk Factor Surveillance System (BRFSS)--a cross-sectional telephone survey that state health departments conduct monthly over landline telephones and cellular telephones with a standardized questionnaire and technical and methodologic assistance from CDC. BRFSS is used to collect prevalence data among adult U.S. residents regarding their risk behaviors and preventive health practices that can affect their health status. Respondent data are forwarded to CDC to be aggregated for each state, returned with standard tabulations, and published at year's end by each state. In 2011, more than 500,000 interviews were conducted in the states, the District of Columbia, and participating U.S. territories and other geographic areas.<br>The files in this deposit were downloaded from the CDC website by Julia Dennett, Yale University, and Toby Chaiken, J-PAL North America, and archived by Travis Donahoe, Harvard University. Additional information edited by Michael Darisse and Lars Vilhuber, Cornell University and American Economic Association.<br><br><br>
DOI: 10.5517/ccdc.csd.cc280hng
title: CCDC 2085855: Experimental Crystal Structure Determination

description: Related Article: Ruiyang Lyu, Curtis E. Moore, Tianyu Liu, Yongze Yu, Yiying Wu|2021|J.Am.Chem.Soc.|143|12766|doi:10.1021/jacs.1c05441
DOI: 10.5517/ccdc.csd.cc27yjlb
title: CCDC 2083962: Experimental Crystal Structure Determination

description: Related Article: Taichi Sotani, Toshiko Mizokuro, Tatsuo Yajima, Hiromitsu Sogawa, Fumio Sanda|2021|Polym.Chem.|12|4829|doi:10.1039/D1PY00665G
DOI: 10.5517/ccdc.csd.cc2887mf
title: CCDC 2093294: Experimental Crystal Structure Determination

description: Related Article: Jinhui Wang, Xinyuan Zhang, Fei Liang, Zhanggui Hu, Yicheng Wu|2021|Dalton Trans.|50|11555|doi:10.1039/D1DT02217B
DOI: 10.5517/ccdc.csd.cc2887ng
title: CCDC 2093295: Experimental Crystal Structure Determination

description: Related Article: Jinhui Wang, Xinyuan Zhang, Fei Liang, Zhanggui Hu, Yicheng Wu|2021|Dalton Trans.|50|11555|doi:10.1039/D1DT02217B
DOI: 10.5517/ccdc.csd.cc2887ph
title: CCDC 2093296: Experimental Crystal Structure Determination

description: Related Article: Jinhui Wang, Xinyuan Zhang, Fei Liang, Zhanggui Hu, Yicheng Wu|2021|Dalton Trans.|50|11555|doi:10.1039/D1DT02217B
DOI: 10.5517/ccdc.csd.cc289783
title: CCDC 2094244: Experimental Crystal Structure Determination

description: Related Article: Guang-Li Wang, Jun Wang, Ling-Peng Zhou, Xinyi Cai, Meiyi Xu, Jingzhe Lin, Mohd. Muddassir, Hiroshi Sakiyama|2021|Inorg.Chim.Acta|527|120566|doi:10.1016/j.ica.2021.120566
DOI: 10.5517/ccdc.csd.cc21pmt6
title: CCDC 1897628: Experimental Crystal Structure Determination

description: Related Article: Lei Li, Yan Zhao, Xiu-Guang Wang, Wei-Chao Song, Zheng-Guo Huang, Xiao-Jun Zhao, En-Cui Yang|2021|Inorg.Chem.Front.|8|4044|doi:10.1039/D1QI00683E
DOI: 10.5517/ccdc.csd.cc21pmv7
title: CCDC 1897629: Experimental Crystal Structure Determination

description: Related Article: Lei Li, Yan Zhao, Xiu-Guang Wang, Wei-Chao Song, Zheng-Guo Huang, Xiao-Jun Zhao, En-Cui Yang|2021|Inorg.Chem.Front.|8|4044|doi:10.1039/D1QI00683E
DOI: 10.5517/ccdc.csd.cc21pmw8
title: CCDC 1897630: Experimental Crystal Structure Determination

description: Related Article: Lei Li, Yan Zhao, Xiu-Guang Wang, Wei-Chao Song, Zheng-Guo Huang, Xiao-Jun Zhao, En-Cui Yang|2021|Inorg.Chem.Front.|8|4044|doi:10.1039/D1QI00683E
DOI: 10.6073/pasta/ec4d18f4766e57564c06eee3d462a46f
title: Lake Sediment Pollen from Benson Pond in Washington MA from 13834 BP to Present

description: Aim We analyzed a dataset composed of multiple palaeoclimate and lake-sediment pollen records from New England to explore how postglacial changes in the composition and spatial patterns of vegetation were controlled by regional-scale climate change, a subregional environmental gradient, and landscape-scale variations in soil characteristics. Location The 120,000-km2 study area includes parts of Vermont and New Hampshire in the north, where sites are 150-200 km from the Atlantic Ocean, and spans the coastline from southeastern New York to Cape Cod and the adjacent islands, including Block Island, the Elizabeth Islands, Nantucket, and Martha’s Vineyard. Results Boreal forest featuring Picea and Pinus banksiana was present across the region when conditions were cool and dry 14,000-12,000 calibrated 14C years before present (ybp). Pinus strobus became regionally dominant as temperatures increased between 12,000 and 10,000 ybp. The composition of forests in inland and coastal areas diverged in response to further warming after 10,000 ybp, when Quercus and Pinus rigida expanded across southern New England, while conditions remained cool enough in inland areas to maintain Pinus strobus. Increasing precipitation allowed Tsuga canadensis, Fagus grandifolia, and Betula to replace Pinus strobus in inland areas during 9000-8000 ybp, and also led to the expansion of Carya across the coastal part of the region beginning at 7000-6000 ybp. Abrupt cooling at 5500-5000 ybp caused sharp declines in Tsuga in inland areas and Quercus at some coastal sites, and the populations of those taxa remained low until they recovered around 3000 ybp in response to rising precipitation. Throughout most of the Holocene, sites underlain by sandy glacial deposits were occupied by Pinus rigida and Quercus. Main conclusions Postglacial changes in the composition and spatial pattern of New England forests were controlled by long-term trends and abrupt shifts in temperature and precipitation, as well as by the environmental gradient between coastal and inland parts of the region. Substrate and soil moisture shaped landscape-scale variations in forest composition.
DOI: 10.6073/pasta/d6854f81ae524b2a1eeab0eaa328b10f
title: Lake Sediment Pollen from Berry Pond in North Andover MA from 13676 BP to Present

description: Aim We analyzed a dataset composed of multiple palaeoclimate and lake-sediment pollen records from New England to explore how postglacial changes in the composition and spatial patterns of vegetation were controlled by regional-scale climate change, a subregional environmental gradient, and landscape-scale variations in soil characteristics. Location The 120,000-km2 study area includes parts of Vermont and New Hampshire in the north, where sites are 150-200 km from the Atlantic Ocean, and spans the coastline from southeastern New York to Cape Cod and the adjacent islands, including Block Island, the Elizabeth Islands, Nantucket, and Martha’s Vineyard. Results Boreal forest featuring Picea and Pinus banksiana was present across the region when conditions were cool and dry 14,000-12,000 calibrated 14C yrs before present (ybp). Pinus strobus became regionally dominant as temperatures increased between 12,000 and 10,000 ybp. The composition of forests in inland and coastal areas diverged in response to further warming after 10,000 ybp, when Quercus and Pinus rigida expanded across southern New England, while conditions remained cool enough in inland areas to maintain Pinus strobus. Increasing precipitation allowed Tsuga canadensis, Fagus grandifolia, and Betula to replace Pinus strobus in inland areas during 9000-8000 ybp, and also led to the expansion of Carya across the coastal part of the region beginning at 7000-6000 ybp. Abrupt cooling at 5500-5000 ybp caused sharp declines in Tsuga in inland areas and Quercus at some coastal sites, and the populations of those taxa remained low until they recovered around 3000 ybp in response to rising precipitation. Throughout most of the Holocene, sites underlain by sandy glacial deposits were occupied by Pinus rigida and Quercus. Main conclusions Postglacial changes in the composition and spatial pattern of New England forests were controlled by long-term trends and abrupt shifts in temperature and precipitation, as well as by the environmental gradient between coastal and inland parts of the region. Substrate and soil moisture shaped landscape-scale variations in forest composition.
DOI: 10.6073/pasta/4760b93e6ce6049bc3748604a2ce6ceb
title: Lake Sediment Pollen from Berry Pond in Hancock MA from 13576 BP to Present

description: Aim We analyzed a dataset composed of multiple palaeoclimate and lake-sediment pollen records from New England to explore how postglacial changes in the composition and spatial patterns of vegetation were controlled by regional-scale climate change, a subregional environmental gradient, and landscape-scale variations in soil characteristics. Location The 120,000-km2 study area includes parts of Vermont and New Hampshire in the north, where sites are 150-200 km from the Atlantic Ocean, and spans the coastline from southeastern New York to Cape Cod and the adjacent islands, including Block Island, the Elizabeth Islands, Nantucket, and Martha’s Vineyard. Results Boreal forest featuring Picea and Pinus banksiana was present across the region when conditions were cool and dry 14,000-12,000 calibrated 14C yrs before present (ybp). Pinus strobus became regionally dominant as temperatures increased between 12,000 and 10,000 ybp. The composition of forests in inland and coastal areas diverged in response to further warming after 10,000 ybp, when Quercus and Pinus rigida expanded across southern New England, while conditions remained cool enough in inland areas to maintain Pinus strobus. Increasing precipitation allowed Tsuga canadensis, Fagus grandifolia, and Betula to replace Pinus strobus in inland areas during 9000-8000 ybp, and also led to the expansion of Carya across the coastal part of the region beginning at 7000-6000 ybp. Abrupt cooling at 5500-5000 ybp caused sharp declines in Tsuga in inland areas and Quercus at some coastal sites, and the populations of those taxa remained low until they recovered around 3000 ybp in response to rising precipitation. Throughout most of the Holocene, sites underlain by sandy glacial deposits were occupied by Pinus rigida and Quercus. Main conclusions Postglacial changes in the composition and spatial pattern of New England forests were controlled by long-term trends and abrupt shifts in temperature and precipitation, as well as by the environmental gradient between coastal and inland parts of the region. Substrate and soil moisture shaped landscape-scale variations in forest composition.
DOI: 10.25405/data.ncl.15180147
title: PiCoBoo database

description: The <b>PiCoBoo </b>project addressed 19th-century European picturebooks printed in colour for children and assessed their significance as a catalyst for major cultural and social changes. It provided the first detailed account of when, where and how these books were made, of who produced them and for what audiences; it analysed what their long-term influence was, across national boundaries, and placed them in larger cultural, publishing and visual histories.The <b>PiCoBoo</b> database has made accessible a large corpus of picturebooks, dispersed across countries and institutions, only partially retrievable through local catalogues, not always correctly described and in a not-uniformed way. Working with network organisations, it has been possible to define cataloguing standards and establish agreed practices for describing children’s picturebooks, thus providing a framework for understanding them.
DOI: 10.6073/pasta/5f9f57bc29ec952b35a6937e5960f07b
title: Lake Sediment Pollen and Charcoal from Black Pond on Martha's Vineyard MA from 9926 BP to Present

description: Aim We analyzed a dataset composed of multiple palaeoclimate and lake-sediment pollen and charcoal records from New England to explore how postglacial changes in forest composition and spatial patterns of vegetation and fire were controlled by regional-scale climate change, a subregional environmental gradient, and landscape-scale variations in soil characteristics. Location The 120,000-km2 study area includes parts of Vermont and New Hampshire in the north, where sites are 150-200 km from the Atlantic Ocean, and spans the coastline from southeastern New York to Cape Cod and the adjacent islands, including Block Island, the Elizabeth Islands, Nantucket, and Martha’s Vineyard. Results Boreal forest featuring Picea and Pinus banksiana was present across the region when conditions were cool and dry 14,000-12,000 calibrated 14C yrs before present (ybp). Pinus strobus became regionally dominant as temperatures increased between 12,000 and 10,000 ybp. The composition of forests in inland and coastal areas diverged in response to further warming after 10,000 ybp, when Quercus and Pinus rigida expanded across southern New England, while conditions remained cool enough in inland areas to maintain Pinus strobus. Fire severity was high during 10,000-8000 ybp. Increasing precipitation allowed Tsuga canadensis, Fagus grandifolia, and Betula to replace Pinus strobus in inland areas during 9000-8000 ybp, and also led to the expansion of Carya across the coastal part of the region beginning at 7000-6000 ybp. Abrupt cooling at 5500-5000 ybp caused sharp declines in Tsuga in inland areas and Quercus at some coastal sites, and the populations of those taxa remained low until they recovered around 3000 ybp in response to rising precipitation. Throughout most of the Holocene, sites underlain by sandy glacial deposits were occupied by Pinus rigida and Quercus. Main conclusions Postglacial changes in the composition and spatial pattern of New England forests were controlled by long-term trends and abrupt shifts in temperature and precipitation, as well as by the environmental gradient between coastal and inland parts of the region. Substrate and soil moisture shaped landscape-scale variations in forest composition. Climate and fuels largely controlled fire severity in New England during the postglacial interval.
DOI: 10.25405/data.ncl.15180186
title: PiCoBoo database: Routledge's new sixpenny toy book series

description: Routledge's new sixpenny toy book series titles
DOI: 10.25405/data.ncl.15180933
title: PiCoBoo database: Aunt Mavor's Picture Books for Little Readers [First Series]

description: Aunt Mavor's Picture Books for Little Readers [First Series]
DOI: 10.25405/data.ncl.15180933.v1
title: PiCoBoo database: Aunt Mavor's Picture Books for Little Readers [First Series]

description: Aunt Mavor's Picture Books for Little Readers [First Series]
DOI: 10.6073/pasta/6ae449e371ad71f2b1252393dd8ff1f9
title: Lake Sediment Pollen and Charcoal from Blaney's Pond in the Elizabeth Islands MA from 13582 BP to Present

description: Aim We analyzed a dataset composed of multiple palaeoclimate and lake-sediment pollen and charcoal records from New England to explore how postglacial changes in forest composition and spatial patterns of vegetation and fire were controlled by regional-scale climate change, a subregional environmental gradient, and landscape-scale variations in soil characteristics. Location The 120,000-km2 study area includes parts of Vermont and New Hampshire in the north, where sites are 150-200 km from the Atlantic Ocean, and spans the coastline from southeastern New York to Cape Cod and the adjacent islands, including Block Island, the Elizabeth Islands, Nantucket, and Martha’s Vineyard. Results Boreal forest featuring Picea and Pinus banksiana was present across the region when conditions were cool and dry 14,000-12,000 calibrated 14C yrs before present (ybp). Pinus strobus became regionally dominant as temperatures increased between 12,000 and 10,000 ybp. The composition of forests in inland and coastal areas diverged in response to further warming after 10,000 ybp, when Quercus and Pinus rigida expanded across southern New England, while conditions remained cool enough in inland areas to maintain Pinus strobus. Fire severity was high during 10,000-8000 ybp. Increasing precipitation allowed Tsuga canadensis, Fagus grandifolia, and Betula to replace Pinus strobus in inland areas during 9000-8000 ybp, and also led to the expansion of Carya across the coastal part of the region beginning at 7000-6000 ybp. Abrupt cooling at 5500-5000 ybp caused sharp declines in Tsuga in inland areas and Quercus at some coastal sites, and the populations of those taxa remained low until they recovered around 3000 ybp in response to rising precipitation. Throughout most of the Holocene, sites underlain by sandy glacial deposits were occupied by Pinus rigida and Quercus. Main conclusions Postglacial changes in the composition and spatial pattern of New England forests were controlled by long-term trends and abrupt shifts in temperature and precipitation, as well as by the environmental gradient between coastal and inland parts of the region. Substrate and soil moisture shaped landscape-scale variations in forest composition. Climate and fuels largely controlled fire severity in New England during the postglacial interval.
DOI: 10.6073/pasta/80f76d0dde7edf67472662e2472eb6e1
title: Lake Sediment Pollen and Charcoal from Blood Pond in Dudley MA from 13874 BP to Present

description: Aim We analyzed a dataset composed of multiple palaeoclimate and lake-sediment pollen and charcoal records from New England to explore how postglacial changes in forest composition and spatial patterns of vegetation and fire were controlled by regional-scale climate change, a subregional environmental gradient, and landscape-scale variations in soil characteristics. Location The 120,000-km2 study area includes parts of Vermont and New Hampshire in the north, where sites are 150-200 km from the Atlantic Ocean, and spans the coastline from southeastern New York to Cape Cod and the adjacent islands, including Block Island, the Elizabeth Islands, Nantucket, and Martha’s Vineyard. Results Boreal forest featuring Picea and Pinus banksiana was present across the region when conditions were cool and dry 14,000-12,000 calibrated 14C yrs before present (ybp). Pinus strobus became regionally dominant as temperatures increased between 12,000 and 10,000 ybp. The composition of forests in inland and coastal areas diverged in response to further warming after 10,000 ybp, when Quercus and Pinus rigida expanded across southern New England, while conditions remained cool enough in inland areas to maintain Pinus strobus. Fire severity was high during 10,000-8000 ybp. Increasing precipitation allowed Tsuga canadensis, Fagus grandifolia, and Betula to replace Pinus strobus in inland areas during 9000-8000 ybp, and also led to the expansion of Carya across the coastal part of the region beginning at 7000-6000 ybp. Abrupt cooling at 5500-5000 ybp caused sharp declines in Tsuga in inland areas and Quercus at some coastal sites, and the populations of those taxa remained low until they recovered around 3000 ybp in response to rising precipitation. Throughout most of the Holocene, sites underlain by sandy glacial deposits were occupied by Pinus rigida and Quercus. Main conclusions Postglacial changes in the composition and spatial pattern of New England forests were controlled by long-term trends and abrupt shifts in temperature and precipitation, as well as by the environmental gradient between coastal and inland parts of the region. Substrate and soil moisture shaped landscape-scale variations in forest composition. Climate and fuels largely controlled fire severity in New England during the postglacial interval.
DOI: 10.25405/data.ncl.15181071
title: PiCoBoo database: Aunt Mavor's Picture Books for Little Readers [Second Series]

description: Aunt Mavor's Picture Books for Little Readers [Second Series]
DOI: 10.25405/data.ncl.15181071.v1
title: PiCoBoo database: Aunt Mavor's Picture Books for Little Readers [Second Series]

description: Aunt Mavor's Picture Books for Little Readers [Second Series]