Epilithic and sestonic chlorophyll for Oksrukuyik Creek during the summers of 1990-2009

Sestonic and epilithic chlorophyll for the Oksrukuyik Creek during the summers of 1990 - 2009. Water was filtered and rocks from designated locations on the Oksrukuyik Creek were scrubbed for epilithic algae approximately three times each summer. Sampling formerly included stations in the fertilized...

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Bibliographic Details
Other Authors: ElissaSchuett, AdrianGreen, KarieSlavik
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:
Ice
Online Access:http://hdl.handle.net/10255/dryad.16168
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.10016.4/xml
id ftdryad:oai:v1.datadryad.org:10255/dryad.16168
record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.16168 2023-05-15T15:13:04+02:00 Epilithic and sestonic chlorophyll for Oksrukuyik Creek during the summers of 1990-2009 ElissaSchuett AdrianGreen KarieSlavik Oksrukuyik Creek, North Slope of Alaska, reference reach and formerly fertilized reach. Distances are based on original 1992 phosphorus dripper and are in stream kilometers. Upstream 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. -149.0973 W -149.0973 E 68.6863 N 68.6863 S -149.75 W -149.0433 E 68.8 N 68.5 S 1990-06-01 to 2009-09-01 2009 text/plain http://hdl.handle.net/10255/dryad.16168 http://metacat.lternet.edu/knb/metacat/knb-lter-arc.10016.4/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.10016.4/xml knb-lter-arc.10016.4 http://hdl.handle.net/10255/dryad.16168 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 Oksrukuyik Creek primary production disturbance dataset 2009 ftdryad 2020-01-01T14:34:54Z Sestonic and epilithic chlorophyll for the Oksrukuyik Creek during the summers of 1990 - 2009. Water was filtered and rocks from designated locations on the Oksrukuyik Creek were scrubbed for epilithic algae approximately three times each summer. Sampling formerly included stations in the fertilized and reference reaches. Current sampling stations are in the reference reach of the stream, upstream of the point of phosphorus addition that occurred from 1991-1996. Sampling dates are typically once in each June, 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
Oksrukuyik Creek
primary production
disturbance
spellingShingle Chlorophyll a
Epilithic Algae
sestonic
Oksrukuyik Creek
primary production
disturbance
Epilithic and sestonic chlorophyll for Oksrukuyik Creek during the summers of 1990-2009
topic_facet Chlorophyll a
Epilithic Algae
sestonic
Oksrukuyik Creek
primary production
disturbance
description Sestonic and epilithic chlorophyll for the Oksrukuyik Creek during the summers of 1990 - 2009. Water was filtered and rocks from designated locations on the Oksrukuyik Creek were scrubbed for epilithic algae approximately three times each summer. Sampling formerly included stations in the fertilized and reference reaches. Current sampling stations are in the reference reach of the stream, upstream of the point of phosphorus addition that occurred from 1991-1996. Sampling dates are typically once in each June, July, and August.
author2 ElissaSchuett
AdrianGreen
KarieSlavik
format Dataset
title Epilithic and sestonic chlorophyll for Oksrukuyik Creek during the summers of 1990-2009
title_short Epilithic and sestonic chlorophyll for Oksrukuyik Creek during the summers of 1990-2009
title_full Epilithic and sestonic chlorophyll for Oksrukuyik Creek during the summers of 1990-2009
title_fullStr Epilithic and sestonic chlorophyll for Oksrukuyik Creek during the summers of 1990-2009
title_full_unstemmed Epilithic and sestonic chlorophyll for Oksrukuyik Creek during the summers of 1990-2009
title_sort epilithic and sestonic chlorophyll for oksrukuyik creek during the summers of 1990-2009
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.16168
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.10016.4/xml
op_coverage Oksrukuyik Creek, North Slope of Alaska, reference reach and formerly fertilized reach. Distances are based on original 1992 phosphorus dripper and are in stream kilometers. Upstream 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.
-149.0973 W -149.0973 E 68.6863 N 68.6863 S
-149.75 W -149.0433 E 68.8 N 68.5 S
1990-06-01 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.10016.4/xml
knb-lter-arc.10016.4
http://hdl.handle.net/10255/dryad.16168
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
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