cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.1204991
title: Lab 4 Week 5

description: The first site of the experiment was the grassland at York University’s Keele campus beside the Pond road. An adult maple tree was randomly selected in the middle of the grassland which was the warmest part of the area. To have been considered an adult tree, the maple tree had to be twice the height of one consistent student, which was about 3.4 metres. The percent open space of the tree (the amount of light the tree received), was found by one student consistently forming a rectangle with the index finger and thumb of both hands joint together. The student would raise this rectangle until it was at the top of the tree where the sun hit the leaves. The approximate measure of their rectangle that was not covered by leaves was recorded as the percent open space. A leaf was then removed from the tree. The length of the leaf from the part where the stem attached to the leaf (but not including the stem length) to the top of the leaf was measured with a transect in metres and recorded. This was repeated two more times for two new leaves from the tree. To measure for density (competition), the distance to the nearest three adult trees of any species was measured with a transect in metres and recorded. This entire procedure of finding a random tree, measuring the amount of light the tree receives and density of trees in the area was repeated for twenty trees (sample size) in the grassland. This was then repeated for twenty trees in the centre of the forest as it was the coolest part of the forest. The total sample size, for both the grassland and forest, was 40 trees.
DOI: 10.6084/m9.figshare.1205063.v1
title: Mameyes River RFID Tracer Cobbles

description: Positions of RFID equiped coarse sediment tracer particles before and after floods at the single flood to annual timescales in the Mameyes River, PR. Please see accompanying metadata file "RFID Tracer Documentation". Tracer particle locations are available in both a cartesian coordinate system, as well as a streamwise normal coordinate system.
DOI: 10.6084/m9.figshare.1205063.v3
title: Mameyes River RFID Tracer Cobbles

description: Positions of RFID equiped coarse sediment tracer particles before and after floods at the single flood to annual timescales in the Mameyes River, PR. Please see accompanying metadata file "RFID Tracer Documentation". Tracer particle locations are available in both a cartesian coordinate system, as well as a streamwise normal coordinate system.
DOI: 10.6084/m9.figshare.1204991.v1
title: Lab 4 Week 5

description: The first site of the experiment was the grassland at York University’s Keele campus beside the Pond road. An adult maple tree was randomly selected in the middle of the grassland which was the warmest part of the area. To have been considered an adult tree, the maple tree had to be twice the height of one consistent student, which was about 3.4 metres. The percent open space of the tree (the amount of light the tree received), was found by one student consistently forming a rectangle with the index finger and thumb of both hands joint together. The student would raise this rectangle until it was at the top of the tree where the sun hit the leaves. The approximate measure of their rectangle that was not covered by leaves was recorded as the percent open space. A leaf was then removed from the tree. The length of the leaf from the part where the stem attached to the leaf (but not including the stem length) to the top of the leaf was measured with a transect in metres and recorded. This was repeated two more times for two new leaves from the tree. To measure for density (competition), the distance to the nearest three adult trees of any species was measured with a transect in metres and recorded. This entire procedure of finding a random tree, measuring the amount of light the tree receives and density of trees in the area was repeated for twenty trees (sample size) in the grassland. This was then repeated for twenty trees in the centre of the forest as it was the coolest part of the forest. The total sample size, for both the grassland and forest, was 40 trees.
DOI: 10.6084/m9.figshare.1204999.v1
title: Author Insights 2014

description: Raw data from Nature Publishing Group and Palgrave Macmillan's annual Author Insights survey. Verbatims and other identifying fields redacted.
DOI: 10.6084/m9.figshare.1204968
title: Impact of reworked foraminifera from an eroding salt marsh on sea-level studies, New Zealand

description: Quantitative sea-level reconstructions using Holocene foraminifera are usually based on transfer function estimates of elevation derived from the tidal-elevation-related zonation of modern salt marsh foraminifera at the same site. Many New Zealand salt marshes are actively eroding as a result of recent sea-level rise exceeding sediment supply, making it difficult to find transects for modern analogue studies that are unaffected by erosion at their seaward ends. At Waikawa Harbour, South Island, New Zealand we show that reworked salt marsh foraminifera from the eroding bank have been mixed in significant quantities with in situ faunas: (1) in the sand flat seaward of the marsh; (2) in the spring tidal marsh on top of the 80-cm-high bank (together with mid tide foraminifera from the sand below the bank); and (3) transported laterally into a nearby non-eroding rush marsh at lower elevation. The fibrous organic-rich salt marsh mud of the bank has been undermined by erosion and large blocks have collapsed to a lower level on the sand flat where the in situ relict faunas are being mixed with newly colonised lower elevation salt marsh foraminifera. These studies show that eroding salt marshes may result in substantial reworking and mixing of foraminiferal tests into the modern faunas thereby compromising their use in sea-level reconstructions. This study prompted us to revisit part of a cored sequence at nearby Catlins Lake and reinterpret a previously inferred earthquake displacement (5–4.5 ka) to be the result of an eroding and collapsing salt marsh bank instead.
DOI: 10.6084/m9.figshare.1204999.v2
title: Author Insights 2014

description: Raw data from Nature Publishing Group and Palgrave Macmillan's annual Author Insights survey. Verbatims and other identifying fields redacted.
DOI: 10.6084/m9.figshare.1204999.v3
title: Author Insights 2014

description: Raw data from Nature Publishing Group and Palgrave Macmillan's annual Author Insights survey. Verbatims and other identifying fields redacted.
DOI: 10.6084/m9.figshare.1204968.v1
title: Impact of reworked foraminifera from an eroding salt marsh on sea-level studies, New Zealand

description: Quantitative sea-level reconstructions using Holocene foraminifera are usually based on transfer function estimates of elevation derived from the tidal-elevation-related zonation of modern salt marsh foraminifera at the same site. Many New Zealand salt marshes are actively eroding as a result of recent sea-level rise exceeding sediment supply, making it difficult to find transects for modern analogue studies that are unaffected by erosion at their seaward ends. At Waikawa Harbour, South Island, New Zealand we show that reworked salt marsh foraminifera from the eroding bank have been mixed in significant quantities with in situ faunas: (1) in the sand flat seaward of the marsh; (2) in the spring tidal marsh on top of the 80-cm-high bank (together with mid tide foraminifera from the sand below the bank); and (3) transported laterally into a nearby non-eroding rush marsh at lower elevation. The fibrous organic-rich salt marsh mud of the bank has been undermined by erosion and large blocks have collapsed to a lower level on the sand flat where the in situ relict faunas are being mixed with newly colonised lower elevation salt marsh foraminifera. These studies show that eroding salt marshes may result in substantial reworking and mixing of foraminiferal tests into the modern faunas thereby compromising their use in sea-level reconstructions. This study prompted us to revisit part of a cored sequence at nearby Catlins Lake and reinterpret a previously inferred earthquake displacement (5–4.5 ka) to be the result of an eroding and collapsing salt marsh bank instead.
DOI: 10.6084/m9.figshare.1204932
title: The effect of Adaptation on the Tuning Curves

description: Thanks for your attention to this paper and dataset. Here you can find data set of extracellular recording from rat auditory cortex (A1). there is a session of our recording available. However, upon request we are very willing to make data available for interested researchers that have no overlapping with our analysis. This two text files are the raw data of four sites that recorded simultaneously by four FHC electrode on four channel of MCS system. The first file is the responses of first sequence (001-5: usual condition) and the second one is the response of second sequence (003-5: adapted condition). In each file, the first column is time (the recording sampling frequency is Fs=10.000). The second to fifth columns show the signal of four recorded channels (voltage of recorded signal). Last column indicates the digital trigger and the onset of stimulus presentation. Each stimulus combination presented 50ms and with 300ms rest time. The paradigm is illustrated in the material and methods part of paper manuscript. Please ask any question about data: moh3enparto@gmail.com
DOI: 10.6084/m9.figshare.1204968.v3
title: Impact of reworked foraminifera from an eroding salt marsh on sea-level studies, New Zealand

description: Quantitative sea-level reconstructions using Holocene foraminifera are usually based on transfer function estimates of elevation derived from the tidal-elevation-related zonation of modern salt marsh foraminifera at the same site. Many New Zealand salt marshes are actively eroding as a result of recent sea-level rise exceeding sediment supply, making it difficult to find transects for modern analogue studies that are unaffected by erosion at their seaward ends. At Waikawa Harbour, South Island, New Zealand we show that reworked salt marsh foraminifera from the eroding bank have been mixed in significant quantities with in situ faunas: (1) in the sand flat seaward of the marsh; (2) in the spring tidal marsh on top of the 80-cm-high bank (together with mid tide foraminifera from the sand below the bank); and (3) transported laterally into a nearby non-eroding rush marsh at lower elevation. The fibrous organic-rich salt marsh mud of the bank has been undermined by erosion and large blocks have collapsed to a lower level on the sand flat where the in situ relict faunas are being mixed with newly colonised lower elevation salt marsh foraminifera. These studies show that eroding salt marshes may result in substantial reworking and mixing of foraminiferal tests into the modern faunas thereby compromising their use in sea-level reconstructions. This study prompted us to revisit part of a cored sequence at nearby Catlins Lake and reinterpret a previously inferred earthquake displacement (5–4.5 ka) to be the result of an eroding and collapsing salt marsh bank instead.
DOI: 10.6084/m9.figshare.1204932.v2
title: The effect of Adaptation on the Tuning Curves

description: Thanks for your attention to this paper and dataset. Here you can find data set of extracellular recording from rat auditory cortex (A1). there is a session of our recording available. However, upon request we are very willing to make data available for interested researchers that have no overlapping with our analysis. This two text files are the raw data of four sites that recorded simultaneously by four FHC electrode on four channel of MCS system. The first file is the responses of first sequence (001-5: usual condition) and the second one is the response of second sequence (003-5: adapted condition). In each file, the first column is time (the recording sampling frequency is Fs=10.000). The second to fifth columns show the signal of four recorded channels (voltage of recorded signal). Last column indicates the digital trigger and the onset of stimulus presentation. Each stimulus combination presented 50ms and with 300ms rest time. The paradigm is illustrated in the material and methods part of paper manuscript. Please ask any question about data: moh3enparto@gmail.com
DOI: 10.6084/m9.figshare.1204968.v2
title: Impact of reworked foraminifera from an eroding salt marsh on sea-level studies, New Zealand

description: Quantitative sea-level reconstructions using Holocene foraminifera are usually based on transfer function estimates of elevation derived from the tidal-elevation-related zonation of modern salt marsh foraminifera at the same site. Many New Zealand salt marshes are actively eroding as a result of recent sea-level rise exceeding sediment supply, making it difficult to find transects for modern analogue studies that are unaffected by erosion at their seaward ends. At Waikawa Harbour, South Island, New Zealand we show that reworked salt marsh foraminifera from the eroding bank have been mixed in significant quantities with in situ faunas: (1) in the sand flat seaward of the marsh; (2) in the spring tidal marsh on top of the 80-cm-high bank (together with mid tide foraminifera from the sand below the bank); and (3) transported laterally into a nearby non-eroding rush marsh at lower elevation. The fibrous organic-rich salt marsh mud of the bank has been undermined by erosion and large blocks have collapsed to a lower level on the sand flat where the in situ relict faunas are being mixed with newly colonised lower elevation salt marsh foraminifera. These studies show that eroding salt marshes may result in substantial reworking and mixing of foraminiferal tests into the modern faunas thereby compromising their use in sea-level reconstructions. This study prompted us to revisit part of a cored sequence at nearby Catlins Lake and reinterpret a previously inferred earthquake displacement (5–4.5 ka) to be the result of an eroding and collapsing salt marsh bank instead.
DOI: 10.6084/m9.figshare.1204932.v1
title: The effect of Adaptation on the Tuning Curves

description: Thanks for your attention to this paper and dataset. Here you can find data set of extracellular recording from rat auditory cortex (A1). there is a session of our recording available. However, upon request we are very willing to make data available for interested researchers that have no overlapping with our analysis. This two text files are the raw data of four sites that recorded simultaneously by four FHC electrode on four channel of MCS system. The first file is the responses of first sequence (usual condition) and the second one is the response of second sequence (adapted condition). In each file, the first column is time (the recording sampling frequency is Fs=10.000). The second to fifth columns show the signal of four recorded channels (voltage of recorded signal). Last column indicates the digital trigger and the onset of stimulus presentation. Each stimulus combination presented 50ms and with 300ms rest time. The paradigm is illustrated in the material and methods part of paper manuscript. Please ask any question about data: moh3enparto@gmail.com
DOI: 10.6084/m9.figshare.1204727
title: Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon

description: All data from the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon" published in PLOS ONE are included in this fileset.
DOI: 10.6084/m9.figshare.1204679
title: DGB Viewshed Maps

description: Close up viewshed maps from the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon"
DOI: 10.6084/m9.figshare.1204676
title: DGB sites Ripley's K analysis with outer edge simulation

description: Data output for Ripley's K analysis of actual DGB sites published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204677
title: DGB Random1 Ripley

description: Ripley's K data output from the first random permuation of DGB sites above 700 m.a.s.l. published in "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204679.v1
title: DGB Viewshed Maps

description: Close up viewshed maps from the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon"
DOI: 10.6084/m9.figshare.1204675
title: KML file (Google Earth) of DGB sites

description: KML file of DGB sites in the Mandara Mountains, Cameroon.
DOI: 10.6084/m9.figshare.1204677.v1
title: DGB Random1 Ripley

description: Ripley's K data output from the first random permuation of DGB sites above 700 m.a.s.l. published in "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204662
title: DGB intervisibility maps

description: Close up of maps showing intervisibility of actual and 10 permutations of random DGB sites published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204675.v1
title: KML file (Google Earth) of DGB sites

description: KML file of DGB sites in the Mandara Mountains, Cameroon.
DOI: 10.6084/m9.figshare.1204676.v1
title: DGB sites Ripley's K analysis with outer edge simulation

description: Data output for Ripley's K analysis of actual DGB sites published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204659
title: Random DGB 1-10 shapefiles

description: Shapefiles of the 10 permutations of DGB sites published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204660
title: DGB intervisibility spreadsheets

description: Data spreadsheets for intervisibility analysis published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204662.v1
title: DGB intervisibility maps

description: Close up of maps showing intervisibility of actual and 10 permutations of random DGB sites published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204674
title: DGB sight lines maps

description: Close up maps of sight lines of DGB sites published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204658
title: Intervisibility lines for Random DGB 1-10

description: These are the spider diagrams for the 10 randomly generated permutations of DGB sites. The diagrams represent potential lines of sight between all locations and were generated in GRASS 6.4.
DOI: 10.6084/m9.figshare.1204660.v1
title: DGB intervisibility spreadsheets

description: Data spreadsheets for intervisibility analysis published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204674.v1
title: DGB sight lines maps

description: Close up maps of sight lines of DGB sites published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204656
title: Intervisibility lines of DGB sites

description: These are the spider diagrams for the actual DGB sites. The diagrams represent potential lines of sight between all locations and were generated in GRASS 6.4.
DOI: 10.6084/m9.figshare.1204658.v1
title: Intervisibility lines for Random DGB 1-10

description: These are the spider diagrams for the 10 randomly generated permutations of DGB sites. The diagrams represent potential lines of sight between all locations and were generated in GRASS 6.4.
DOI: 10.6084/m9.figshare.1204659.v1
title: Random DGB 1-10 shapefiles

description: Shapefiles of the 10 permutations of DGB sites published in the paper "Analysis of Feature Intervisibility and Cumulative Visibility Using GIS, Bayesian and Spatial Statistics: A Case Study from the Mandara Mountains, Northern Cameroon."
DOI: 10.6084/m9.figshare.1204655
title: 700 m.a.s.l. contour line, Mandara Mountains, Cameroon

description: This is the 700 m.a.s.l. contour lne generated from the DEM of the project area. Random permutations of DGB sites were generated above this elevational contraint.
DOI: 10.6084/m9.figshare.1204657
title: Shapefile of DGB sites

description: Shapefile of the actual locations of DGB sites in the Mandara Mountains, Cameroon.
DOI: 10.6084/m9.figshare.1203646
title: CRAWDAD wireless network data citation bibliography

description: This BibTeX file contains the corpus of papers that cite CRAWDAD wireless network datasets, as used in the paper: Tristan Henderson and David Kotz. Data citation practices in the CRAWDAD wireless network data archive. Proceedings of the Second Workshop on Linking and Contextualizing Publications and Datasets, London, UK, September 2014. Most of the fields are standard BibTeX fields. There are two that require further explanation. "citations" - this field contains the citations for a paper as counted<br>by Google Scholar as of 24 September 2014. "keywords" - this field contains a set of tags indicating data citation practice. These are as follows:<br>- "uses_crawdad_data" - this paper uses a CRAWDAD dataset<br>- "cites_insufficiently" - this paper does not meet our sufficiency criteria<br>- "cites_by_description" - this paper cites a dataset by description rather than dataset identifier<br>- "cites_canonical_paper" - this paper cites the original ("canonical") paper that collected a dataset, rather than pointing to the dataset<br>- "cites_by_name" - this paper cites a dataset by a colloquial name rather than dataset identifier<br>- "cites_crawdad_url" - this paper cites the main CRAWDAD URL rather than a particular dataset<br>- "cites_without_url" - this paper does not provide a URL for dataset access<br>- "cites_wrong_attribution" - this paper attributes a dataset to CRAWDAD, Dartmouth etc rather than the dataset authors<br>- "cites_vaguely" - this paper cites the used datasets (if any) too vaguely to be sufficient If you have any questions about the data, please contact us at<br>crawdad@crawdad.org
DOI: 10.6084/m9.figshare.1204655.v1
title: 700 m.a.s.l. contour line, Mandara Mountains, Cameroon

description: This is the 700 m.a.s.l. contour lne generated from the DEM of the project area. Random permutations of DGB sites were generated above this elevational contraint.
DOI: 10.6084/m9.figshare.1203624
title: All files

description: All files used in paper Nascimento et al. 2015 (42:1349–1357) Reanalysis of the biogeographical hypothesis of range expansion between robust and gracile capuchin monkeys. Journal of Biogeography (DOI: 10.1111/jbi.12448).