id ftdryad:oai:v1.datadryad.org:10255/dryad.11902
record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.11902 2023-05-15T15:53:35+02:00 Biomass of stream macroinvertebrates and benthic organic material in CPCRW The tributary basins of Caribou Creek are all arbitrarily designated with a "C". The C2 basin is the sub-basin with the least amount of permafrost of the CPCRW sub-basins. As such, it has been often been studied intensively in conjunction with C3, the sub-basin with the greatest amount of permafrost. The basin trends to the south, with well-drained slopes and permafrost-underlain treeless muskeg in valley bottom. Although an extensive fire history has not been done, there was probably a stand-replacing fire early in this century (ca. 1925), with some large white spruce stands that survived from the earlier vegetation. -147.603928 W -147.482385 E 65.15876438 N 65.14329713 S 1995-06-01 to 1996-06-29 1995-06-01 to 1996-06-29 1997-08-26 text/plain http://hdl.handle.net/10255/dryad.11902 http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.24.8/xml unknown Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251 http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.24.8/xml knb-lter-bnz.24.8 http://hdl.handle.net/10255/dryad.11902 Access to Data While metadata will be freely available to those requesting it, the data manager will assure that any restrictions on access to data sets in the database will be enforced. Data will not be released without proper permission first being obtained from the investigator who generated the data. Use of data Researchers should receive adequate acknowledgment for the use of their data by others and should be provided with copies of publications using their data. Users of data from the data base must be aware that data is not to be sold or redistributed.Citing Bonanza Creek LTER DatasetsIt is considered a matter of professional ethics to acknowledge the work of other scientists. Thus, the Data User will properly cite the Data Set in any publications or in the metadata of any derived data products that were produced using the Data Set. caribou poker creeks research watershed (CPCRW) macroinvertebrates stream ecology community subarctic benthic organic matter dataset 1997 ftdryad 2020-01-01T14:26:38Z Dataset Caribou-Poker Creeks Research Watershed permafrost Subarctic Dryad Digital Repository (Duke University)
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic caribou poker creeks research watershed (CPCRW)
macroinvertebrates
stream ecology
community
subarctic
benthic
organic matter
spellingShingle caribou poker creeks research watershed (CPCRW)
macroinvertebrates
stream ecology
community
subarctic
benthic
organic matter
Biomass of stream macroinvertebrates and benthic organic material in CPCRW
topic_facet caribou poker creeks research watershed (CPCRW)
macroinvertebrates
stream ecology
community
subarctic
benthic
organic matter
format Dataset
title Biomass of stream macroinvertebrates and benthic organic material in CPCRW
title_short Biomass of stream macroinvertebrates and benthic organic material in CPCRW
title_full Biomass of stream macroinvertebrates and benthic organic material in CPCRW
title_fullStr Biomass of stream macroinvertebrates and benthic organic material in CPCRW
title_full_unstemmed Biomass of stream macroinvertebrates and benthic organic material in CPCRW
title_sort biomass of stream macroinvertebrates and benthic organic material in cpcrw
publisher Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251
publishDate 1997
url http://hdl.handle.net/10255/dryad.11902
http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.24.8/xml
op_coverage The tributary basins of Caribou Creek are all arbitrarily designated with a "C". The C2 basin is the sub-basin with the least amount of permafrost of the CPCRW sub-basins. As such, it has been often been studied intensively in conjunction with C3, the sub-basin with the greatest amount of permafrost. The basin trends to the south, with well-drained slopes and permafrost-underlain treeless muskeg in valley bottom. Although an extensive fire history has not been done, there was probably a stand-replacing fire early in this century (ca. 1925), with some large white spruce stands that survived from the earlier vegetation.
-147.603928 W -147.482385 E 65.15876438 N 65.14329713 S
1995-06-01 to 1996-06-29
1995-06-01 to 1996-06-29
genre Caribou-Poker Creeks Research Watershed
permafrost
Subarctic
genre_facet Caribou-Poker Creeks Research Watershed
permafrost
Subarctic
op_relation http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.24.8/xml
knb-lter-bnz.24.8
http://hdl.handle.net/10255/dryad.11902
op_rights Access to Data While metadata will be freely available to those requesting it, the data manager will assure that any restrictions on access to data sets in the database will be enforced. Data will not be released without proper permission first being obtained from the investigator who generated the data. Use of data Researchers should receive adequate acknowledgment for the use of their data by others and should be provided with copies of publications using their data. Users of data from the data base must be aware that data is not to be sold or redistributed.Citing Bonanza Creek LTER DatasetsIt is considered a matter of professional ethics to acknowledge the work of other scientists. Thus, the Data User will properly cite the Data Set in any publications or in the metadata of any derived data products that were produced using the Data Set.
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