Epilithic and sestonic chlorophyll for the Kuparuk River during the summers of 1983 - 2009

Sestonic and epilithic chlorophyll for the Kuparuk River during the summers of 1983 - 2009. Water was filtered and rocks from designated locations on the Kuparuk River were scrubbed for epilithic algae approximately three times each summer. Station sites are relative distance from the original 1983...

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Bibliographic Details
Other Authors: AdrianGreen, KarieSlavik, MichaelMiller, WilWollheim, ElissaSchuett
Format: Dataset
Language:unknown
Published: ARC LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7496arc_im@mbl.eduhttp://ecosystems.mbl.edu/ARC/ 2009
Subjects:
Chlorophyll a
Epilithic Algae
sestonic
Kuparuk River
primary production
Arctic
Northern Foothills
Brooks Range
Dwarf birch
Ice
north slope
permafrost
Tundra
Alaska
Online Access:http://hdl.handle.net/10255/dryad.32274
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1282.6/xml
id ftdryad:oai:v1.datadryad.org:10255/dryad.32274
record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.32274 2023-05-15T15:14:06+02:00 Epilithic and sestonic chlorophyll for the Kuparuk River during the summers of 1983 - 2009 AdrianGreen KarieSlavik MichaelMiller WilWollheim ElissaSchuett Kuparuk River, original 1983 dripper location from which all other sampling station locations are based. Station name is 0.0k. Distances are stream kilometersUpstream stations are negative, downstream are positive. The Arctic LTER research site (68°N and 149°W) is in the foothills region of the North Slope of Alaska and includes the entire Toolik Lake watershed and the adjacent watershed of the upper Kuparuk River, down to the confluence of these two watersheds. This area is typical of the northern foothills of the Brooks Range, with continuous permafrost, no trees, a complete snow cover for 7 to 9 months, winter ice cover on lakes, streams, and ocean, and cessation of river flow during the winter. Tussock tundra vegetation of sedges and grasses mixed with dwarf birch and low willows form the dominant vegetation type with areas of drier heath tundra on ridge tops and other well-drained sites as well as areas of river-bottom willow communities. -149ø23'39.57205" W -149ø23'39.57205" E 68ø38'20.77349" N 68ø38'20.77349" S -149.75 W -149.0433 E 68.8 N 68.5 S 1983-07-22 to 2009-09-01 2009 text/plain http://hdl.handle.net/10255/dryad.32274 http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1282.6/xml unknown ARC LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7496arc_im@mbl.eduhttp://ecosystems.mbl.edu/ARC/ http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1282.6/xml knb-lter-arc.1282.6 http://hdl.handle.net/10255/dryad.32274 Acceptance and utilization of LTER data requires that:The Principal Investigator be sent a notice stating reasons for acquiring any data and a description of the publication intentions.The Principal Investigator of the data set be sent a copy of the report or manuscript prior to submission and be adequately cited in any resultant publicationsA copy of any resultant publications should be sent to: Principal Investigator Ecosystems Center Marine Biological Laboratory Woods Hole, MA 02543 Chlorophyll a Epilithic Algae sestonic Kuparuk River primary production dataset 2009 ftdryad 2020-01-01T14:52:49Z Sestonic and epilithic chlorophyll for the Kuparuk River during the summers of 1983 - 2009. Water was filtered and rocks from designated locations on the Kuparuk River were scrubbed for epilithic algae approximately three times each summer. Station sites are relative distance from the original 1983 phosphorus dripper. Stations include sites in a reference reach, a reach that has been recovering from phosphorus addition since 1996, and a reach that has had phosphorus added since 1983. Phosphoric acid is added to the stream to increase the soluble reactive phosphorus by 0.32 uM. Sampling dates are typically once in June prior to the addition of phosphoric acid and once each in July and August. Dataset Arctic Brooks Range Dwarf birch Ice north slope permafrost Tundra Alaska Dryad Digital Repository (Duke University) Arctic Northern Foothills ENVELOPE(163.917,163.917,-74.733,-74.733)
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic Chlorophyll a
Epilithic Algae
sestonic
Kuparuk River
primary production
spellingShingle Chlorophyll a
Epilithic Algae
sestonic
Kuparuk River
primary production
Epilithic and sestonic chlorophyll for the Kuparuk River during the summers of 1983 - 2009
topic_facet Chlorophyll a
Epilithic Algae
sestonic
Kuparuk River
primary production
description Sestonic and epilithic chlorophyll for the Kuparuk River during the summers of 1983 - 2009. Water was filtered and rocks from designated locations on the Kuparuk River were scrubbed for epilithic algae approximately three times each summer. Station sites are relative distance from the original 1983 phosphorus dripper. Stations include sites in a reference reach, a reach that has been recovering from phosphorus addition since 1996, and a reach that has had phosphorus added since 1983. Phosphoric acid is added to the stream to increase the soluble reactive phosphorus by 0.32 uM. Sampling dates are typically once in June prior to the addition of phosphoric acid and once each in July and August.
author2 AdrianGreen
KarieSlavik
MichaelMiller
WilWollheim
ElissaSchuett
format Dataset
title Epilithic and sestonic chlorophyll for the Kuparuk River during the summers of 1983 - 2009
title_short Epilithic and sestonic chlorophyll for the Kuparuk River during the summers of 1983 - 2009
title_full Epilithic and sestonic chlorophyll for the Kuparuk River during the summers of 1983 - 2009
title_fullStr Epilithic and sestonic chlorophyll for the Kuparuk River during the summers of 1983 - 2009
title_full_unstemmed Epilithic and sestonic chlorophyll for the Kuparuk River during the summers of 1983 - 2009
title_sort epilithic and sestonic chlorophyll for the kuparuk river during the summers of 1983 - 2009
publisher ARC LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7496arc_im@mbl.eduhttp://ecosystems.mbl.edu/ARC/
publishDate 2009
url http://hdl.handle.net/10255/dryad.32274
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1282.6/xml
op_coverage Kuparuk River, original 1983 dripper location from which all other sampling station locations are based. Station name is 0.0k. Distances are stream kilometersUpstream stations are negative, downstream are positive.
The Arctic LTER research site (68°N and 149°W) is in the foothills region of the North Slope of Alaska and includes the entire Toolik Lake watershed and the adjacent watershed of the upper Kuparuk River, down to the confluence of these two watersheds. This area is typical of the northern foothills of the Brooks Range, with continuous permafrost, no trees, a complete snow cover for 7 to 9 months, winter ice cover on lakes, streams, and ocean, and cessation of river flow during the winter. Tussock tundra vegetation of sedges and grasses mixed with dwarf birch and low willows form the dominant vegetation type with areas of drier heath tundra on ridge tops and other well-drained sites as well as areas of river-bottom willow communities.
-149ø23'39.57205" W -149ø23'39.57205" E 68ø38'20.77349" N 68ø38'20.77349" S
-149.75 W -149.0433 E 68.8 N 68.5 S
1983-07-22 to 2009-09-01
long_lat ENVELOPE(163.917,163.917,-74.733,-74.733)
geographic Arctic
Northern Foothills
geographic_facet Arctic
Northern Foothills
genre Arctic
Brooks Range
Dwarf birch
Ice
north slope
permafrost
Tundra
Alaska
genre_facet Arctic
Brooks Range
Dwarf birch
Ice
north slope
permafrost
Tundra
Alaska
op_relation http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1282.6/xml
knb-lter-arc.1282.6
http://hdl.handle.net/10255/dryad.32274
op_rights Acceptance and utilization of LTER data requires that:The Principal Investigator be sent a notice stating reasons for acquiring any data and a description of the publication intentions.The Principal Investigator of the data set be sent a copy of the report or manuscript prior to submission and be adequately cited in any resultant publicationsA copy of any resultant publications should be sent to: Principal Investigator Ecosystems Center Marine Biological Laboratory Woods Hole, MA 02543
_version_ 1766344602401374208

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