cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6073/pasta/53eef3e82b8ca7cbabd115b1074527c0
title: Lake Sediment Pollen and Charcoal from Umpawaug Pond in Redding CT from 9377 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: 10.6084/m9.figshare.24199089.v1
title: Citation count CSV dataset of all DOI bibliographic resources in OpenCitations Index

description: A CSV dataset containing the number of incoming citations to each bibliographic entity identified by a DOI in the OpenCitations Index (https://opencitations.net/index).The dataset is based on the last release of the OpenCitations Index (https://opencitations.net/download) – January 2023. The size of the zipped archive is 0.768 GB, while the size of the unzipped CSV file is 1.9 GB.The CSV dataset contains the citation count of 63,960,029 bibliographic entities. The first column lists the entities, while the second column indicates the corresponding number of incoming citations.
DOI: 10.6073/pasta/345e08b62c08680eb7490a84d3513b0f
title: Lake Sediment Pollen and Charcoal from Uncle Seth's Pond on Martha's Vineyard MA from 13389 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: 10.5523/bris.o27el0rtlqzy2bzyvptq1ofkq
title: State anxiety and emotional face recognition in healthy volunteers (study three - online task), Version 1.1

description: An online observational study investigating the association between state/trait anxiety and emotional face recognition. Healthy adults (n = 2006) completed a six alternated forced choice task in which they were presented with basic emotional expressions (anger, disgust, fear, happiness, sadness and surprise) and were required to identify the emotion present in the face. Outcome measures were recognition accuracy and unbiased hit rate (i.e., sensitivity).

This dataset replaces DOI: 10.5523/bris.112g2vkxomjoo1l26vjmvnlexj
DOI: 10.57693/tn8jwo/d3kiph
title: 03_InclusiveIDSurvey_Data_EN_v1.0.tab

description: Dataset in Serbian. Questionnaire is not available.
DOI: 10.57693/tn8jwo
title: From Inclusive Identities to Inclusive Societies: Exploring Complex Social Identity in the Western Balkans

description: In post-conflict societies the mayor disparities reflect the specific ethnic and religious composition and give evidence of institutionalized discrimination. Minority groups are often socially deprived with unequal access to resources. A great deal of recent social-psychological research repeatedly confirms a strong connection between the inclusiveness of individuals’ identities with their support for inclusiveness of the society as a whole (Bodenhausen, 2010). In order to enhance regional and in-country cohesion, more inclusive religious and ethnic identities as well as alternative identities (European, regional, gender, subcultural) need to be cultivated, beside ethnic and religious ones. One important route to it is to define the conditions that foster complex social identity (SIC). The relevant research has demonstrated that people with more complex social identities show higher inter-group tolerance, are more ready to volunteer and be socially active and also, are more likely to endorse social policies relevant to outgroups. This project aims to develop a complex research design intended to deeply explore antecedents and consequences of SIC in the selected countries. Main Objectives were: 1. To explore via interviews the nature and structure of social identity among young people in Western Balkan countries; establish similarities and differences in different social contexts (different countries, different microenvironments – ethnically homogenous or heterogeneous, from the perspective of minority or majority, different socio-demographic background); 2. To explore the relationships between social identity complexity and a number of socially relevant attitudes and behaviours: social dominance orientation, political cynicism, trust in institutions, conservatism-liberalism, attitudes and distance towards out-groups, attitudes toward antidiscrimination policy (i.e. affirmative action) and civic activism; 3.To define contexts that foster complex social identity
DOI: 10.5281/zenodo.10361266
title: Trained model weights for feedback attention CNNs
DOI: 10.5281/zenodo.10361267
title: Trained model weights for feedback attention CNNs
DOI: 10.6073/pasta/977387bb42eccd9de48c182312736fd1
title: Lake Sediment Pollen and Charcoal from Ware Pond in Marblehead MA from 11218 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: 10.5281/zenodo.10355717
title: Suicide in adolescence: the role of perceived depression, attraction to life and repulsion to life

description: This database includes the raw data linked with the paper "Suicide in adolescence: the role of perceived depression, attraction to life and repulsion to life" published on "JOURNAL NAME". 
In this paper, we reported the results of two self-report questionnaires (BDI-SF, MAST) filled in by adolescent patients with suicidal ideation and suicide attempts. We aimed to assess if self-report questionnaires can predict the possibility that a teenager may commit suicide.
Methods
We included 92 adolescent patients and divided them into two groups according to the interview C-SSRS: patients who present suicidal ideation only and the second consisting of patients presenting suicidal attempts (i.e. who presented concrete and/or interrupted attempts). They filled in the BDI-SF and the MAST.
Results (in brief):
Significant differences were found between the two groups regarding all the scales of the MAST except for the scale "repulsion to death"; the suicidal ideation group showed a greater attraction to life and less attraction to death, as well as less repulsion to life. Furthermore, as attraction to life increases, both repulsion by life and attraction to death decrease, while as the attraction to death increases, so does the repulsion by life. As the suicidal behavior group reported significantly higher levels of depression than the suicidal ideation group, the BDI-SF assumes a predictive function. Finally, the comparison of the two questionnaires highlighted that higher levels of attraction to life correspond to lower levels of depression, as well as higher levels of attraction to death correspond to higher levels of depression.
DOI: 10.5281/zenodo.10355718
title: Suicide in adolescence: the role of perceived depression, attraction to life and repulsion to life

description: This database includes the raw data linked with the paper "Suicide in adolescence: the role of perceived depression, attraction to life and repulsion to life" published on "JOURNAL NAME". 
In this paper, we reported the results of two self-report questionnaires (BDI-SF, MAST) filled in by adolescent patients with suicidal ideation and suicide attempts. We aimed to assess if self-report questionnaires can predict the possibility that a teenager may commit suicide.
Methods
We included 92 adolescent patients and divided them into two groups according to the interview C-SSRS: patients who present suicidal ideation only and the second consisting of patients presenting suicidal attempts (i.e. who presented concrete and/or interrupted attempts). They filled in the BDI-SF and the MAST.
Results (in brief):
Significant differences were found between the two groups regarding all the scales of the MAST except for the scale "repulsion to death"; the suicidal ideation group showed a greater attraction to life and less attraction to death, as well as less repulsion to life. Furthermore, as attraction to life increases, both repulsion by life and attraction to death decrease, while as the attraction to death increases, so does the repulsion by life. As the suicidal behavior group reported significantly higher levels of depression than the suicidal ideation group, the BDI-SF assumes a predictive function. Finally, the comparison of the two questionnaires highlighted that higher levels of attraction to life correspond to lower levels of depression, as well as higher levels of attraction to death correspond to higher levels of depression.
DOI: 10.6073/pasta/32cb0d972b62df6c17aaba0b7e4396ce
title: Lake Sediment Pollen and Charcoal from West Side Pond in Goshen CT from 13397 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/249964bea4b540cd578800322bd10b5a
title: Lake Sediment Pollen from Winneconnet Pond in Norton MA from 13865 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: 10.17632/s37fhsnpd9.2
title: databases for "Lithium-rich basement brines: activity versus concentration geothermometry"

description: Implemented Pitzer and pygcc thermodynamic datasets for PhreeqcI version 3 (Parkhurst and Appelo, 2013) and the The Geochemist’s Workbench version 7 (Bethke and Yeakel, 2007). The Microsoft® Excel file containing best fittings of the logK versus temperature values of the equation 1÷4 is also enclosed in the zip file
DOI: 10.17632/s37fhsnpd9.3
title: databases for "Lithium-rich basement brines: activity versus concentration geothermometry"

description: Implemented Pitzer and pygcc thermodynamic datasets for PhreeqcI version 3 (Parkhurst and Appelo, 2013) and the The Geochemist’s Workbench®, version 7 (Bethke and Yeakel, 2007). The Microsoft® Excel file containing best fittings of the logK versus temperature values of the equation 1÷4 is also enclosed in the zip file
DOI: 10.17632/s37fhsnpd9.1
title: databases for "Lithium-rich basement brines: activity versus concentration geothermometry"

description: Implemented Pitzer and pygcc thermodynamic datasets for PhreeqcI version 3 (Parkhurst and Appelo, 2013) and the The Geochemist’s Workbench version 7 (Bethke and Yeakel, 2007). The Microsoft® Excel file containing best fittings of the logK versus temperature values of the equation 1÷4 is also enclosed in the zip file
DOI: 10.17632/s37fhsnpd9.4
title: databases for "Lithium-rich basement brines: activity versus concentration geothermometry"

description: Implemented Pitzer and pygcc thermodynamic datasets for PhreeqcI version 3 (Parkhurst and Appelo, 2013) and the The Geochemist’s Workbench®, version 7 (Bethke and Yeakel, 2007). The Microsoft® Excel file containing best fittings of the logK versus temperature values of the equation 1÷4 is also enclosed in the zip file.
For details, please see the manuscript Boschetti et al. 2024 "Lithium-rich basement brines: activity versus concentration geothermometry" on Geothermics (Elsevier).
DOI: 10.6073/pasta/1a49607a48d985e64b595bc43c5146d7
title: Lake Sediment Charcoal from Ponds in Southern New England from 14000 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.