Automated Tools for Layer Recognition (BMPix) and Counting (PEAK) ...
We present tools for rapid and quantitative detection of sediment lamination. The BMPix tool extracts color and gray-scale curves from images at pixel resolution. The PEAK tool uses the gray-scale curve and performs, for the first time, fully automated counting of laminae based on three methods. The...
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Online Access: | https://dx.doi.org/10.1594/pangaea.729700 https://doi.pangaea.de/10.1594/PANGAEA.729700 |
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ftdatacite:10.1594/pangaea.729700 2023-10-01T03:50:49+02:00 Automated Tools for Layer Recognition (BMPix) and Counting (PEAK) ... Weber, Michael E Reichelt, Lucia Kuhn, Gerhard Pfeiffer, Miriam Korff, Björn Thurow, Juergen W Ricken, Werner 2010 application/zip https://dx.doi.org/10.1594/pangaea.729700 https://doi.pangaea.de/10.1594/PANGAEA.729700 en eng PANGAEA https://dx.doi.org/10.1029/2009gc002611 https://dx.doi.org/10.1594/pangaea.775955 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Dataset Supplementary Dataset dataset 2010 ftdatacite https://doi.org/10.1594/pangaea.72970010.1029/2009gc00261110.1594/pangaea.775955 2023-09-04T14:52:34Z We present tools for rapid and quantitative detection of sediment lamination. The BMPix tool extracts color and gray-scale curves from images at pixel resolution. The PEAK tool uses the gray-scale curve and performs, for the first time, fully automated counting of laminae based on three methods. The maximum count algorithm counts every bright peak of a couplet of two laminae (annual resolution) in a smoothed curve. The zero-crossing algorithm counts every positive and negative halfway-passage of the curve through a wide moving average, separating the record into bright and dark intervals (seasonal resolution). The same is true for the frequency truncation method, which uses Fourier transformation to decompose the curve into its frequency components before counting positive and negative passages.We applied the new methods successfully to tree rings, to well-dated and already manually counted marine varves from Saanich Inlet, and to marine laminae from the Antarctic continental margin. In combination with ... : This is version 1 of the software as published in 2010. It contains 3 macro files (excel) and a read-me file (pdf) in a zip-archive. To download the updated version 2 of the software as of February 2012, see "Other version". ... Dataset Antarc* Antarctic Arctic Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic Antarctic The Antarctic |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
spellingShingle |
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Weber, Michael E Reichelt, Lucia Kuhn, Gerhard Pfeiffer, Miriam Korff, Björn Thurow, Juergen W Ricken, Werner Automated Tools for Layer Recognition (BMPix) and Counting (PEAK) ... |
topic_facet |
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
We present tools for rapid and quantitative detection of sediment lamination. The BMPix tool extracts color and gray-scale curves from images at pixel resolution. The PEAK tool uses the gray-scale curve and performs, for the first time, fully automated counting of laminae based on three methods. The maximum count algorithm counts every bright peak of a couplet of two laminae (annual resolution) in a smoothed curve. The zero-crossing algorithm counts every positive and negative halfway-passage of the curve through a wide moving average, separating the record into bright and dark intervals (seasonal resolution). The same is true for the frequency truncation method, which uses Fourier transformation to decompose the curve into its frequency components before counting positive and negative passages.We applied the new methods successfully to tree rings, to well-dated and already manually counted marine varves from Saanich Inlet, and to marine laminae from the Antarctic continental margin. In combination with ... : This is version 1 of the software as published in 2010. It contains 3 macro files (excel) and a read-me file (pdf) in a zip-archive. To download the updated version 2 of the software as of February 2012, see "Other version". ... |
format |
Dataset |
author |
Weber, Michael E Reichelt, Lucia Kuhn, Gerhard Pfeiffer, Miriam Korff, Björn Thurow, Juergen W Ricken, Werner |
author_facet |
Weber, Michael E Reichelt, Lucia Kuhn, Gerhard Pfeiffer, Miriam Korff, Björn Thurow, Juergen W Ricken, Werner |
author_sort |
Weber, Michael E |
title |
Automated Tools for Layer Recognition (BMPix) and Counting (PEAK) ... |
title_short |
Automated Tools for Layer Recognition (BMPix) and Counting (PEAK) ... |
title_full |
Automated Tools for Layer Recognition (BMPix) and Counting (PEAK) ... |
title_fullStr |
Automated Tools for Layer Recognition (BMPix) and Counting (PEAK) ... |
title_full_unstemmed |
Automated Tools for Layer Recognition (BMPix) and Counting (PEAK) ... |
title_sort |
automated tools for layer recognition (bmpix) and counting (peak) ... |
publisher |
PANGAEA |
publishDate |
2010 |
url |
https://dx.doi.org/10.1594/pangaea.729700 https://doi.pangaea.de/10.1594/PANGAEA.729700 |
geographic |
Arctic Antarctic The Antarctic |
geographic_facet |
Arctic Antarctic The Antarctic |
genre |
Antarc* Antarctic Arctic Sea ice |
genre_facet |
Antarc* Antarctic Arctic Sea ice |
op_relation |
https://dx.doi.org/10.1029/2009gc002611 https://dx.doi.org/10.1594/pangaea.775955 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.72970010.1029/2009gc00261110.1594/pangaea.775955 |
_version_ |
1778528082696601600 |