Stable isotope (carbon and nitrogen) data for functional groups in the Plum Island Sound Estuary.

Stable isotopes of primary producers will be compared to stable isotopes of functional groups of organisms at primarily three sites within the estuary that have different dominant sources of organic matter. The three sites are: Lower (IBYC, SO-3, mouth of Plum Island Sound, 2-3 km upstream of the mo...

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Bibliographic Details
Other Authors: CharlesHopkinson, HapGarritt
Format: Dataset
Language:unknown
Published: Plum Island Ecosystems LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7485pie_im@mbl.eduhttp://ecosystems.mbl.edu/PIE/ 2004
Subjects:
Online Access:http://hdl.handle.net/10255/dryad.15387
http://metacat.lternet.edu/knb/metacat/knb-lter-pie.13.4/xml
id ftdryad:oai:v1.datadryad.org:10255/dryad.15387
record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.15387 2023-05-15T17:14:23+02:00 Stable isotope (carbon and nitrogen) data for functional groups in the Plum Island Sound Estuary. CharlesHopkinson HapGarritt P2 P5 Old Town Landing Nelson Island IBYC The Plum Island Ecosystems (PIE) LTER site, is located in northeastern Massachusetts, 42.72 N, 70.85 W. The PIE LTER lies at the interface of a thinly soiled, formerly glaciated New England land mass and the highly productive Gulf of Maine. Three watersheds comprise the estuarine drainage basin: Parker (155 km2), Rowley (26 km2) and Ipswich (404 km2). The Ipswich River watershed is highly urbanized with Boston "bedroom" communities encroaching in the headwater region while the Parker is less urbanized and retains a higher proportion of forest. -70.91732887 W -70.91732887 E 42.74988851 N 42.74988851 S -70.87290193 W -70.87290193 E 42.75506932 N 42.75506932 S -70.8365313 W -70.8365313 E 42.76236849 N 42.76236849 S -70.8210343 W -70.8210343 E 42.74691643 N 42.74691643 S -70.79657702 W -70.79657702 E 42.70899476 N 42.70899476 S -71.2198 W -70.7568 E 42.8276 N 42.4965 S 1999-08-23 to 2008-09-24 2004 text/plain http://hdl.handle.net/10255/dryad.15387 http://metacat.lternet.edu/knb/metacat/knb-lter-pie.13.4/xml unknown Plum Island Ecosystems LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7485pie_im@mbl.eduhttp://ecosystems.mbl.edu/PIE/ http://metacat.lternet.edu/knb/metacat/knb-lter-pie.13.4/xml knb-lter-pie.13.4 http://hdl.handle.net/10255/dryad.15387 Acceptance and utilization of PIE-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 PIE LTER organic matter population dynamics Massachusetts stable isotope nitrogen carbon food web trophic fish invertebrates organic particulate zooplankton algae dataset 2004 ftdryad 2020-01-01T14:33:28Z Stable isotopes of primary producers will be compared to stable isotopes of functional groups of organisms at primarily three sites within the estuary that have different dominant sources of organic matter. The three sites are: Lower (IBYC, SO-3, mouth of Plum Island Sound, 2-3 km upstream of the mouth of the estuary), Middle (OTL, PR-10.5, upper Sound, lower Parker, 8-11 km upstream of the mouth of the estuary) and Upper (P2, PR-22, upper Parker, above Middle Rd Bridge (22 km upstream of the mouth odf the estuary). The Lower site is dominated by marine phytoplankton, the Middle site is dominated by a mixture of salt marsh and phytoplankton and the Upper site is dominated by oligohaline phytoplankton and fresh marsh. Ten functional groups will be sampled at each site (Surface sediment, benthic diatoms, Nereis, mummichog, ribbed mussels, POM, blue mussels, pelagic copepods (Acartia), silversides and soft shell clams (Mya). Marsh, benthic algae and phytoplankton inputs or benthic vs. pelagic pathways will be evident in the isotopic signals of these functional groups. Samples will be collected between the middle and end of August to reflect a growing season using recently produced OM. Samples of 15 – 20 individuals will be pooled for analysis. Silversides will have 3 different pooled samples for determination of variance. Dataset Nelson Island Copepods Dryad Digital Repository (Duke University)
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic PIE LTER
organic matter
population dynamics
Massachusetts
stable isotope
nitrogen
carbon
food web
trophic
fish
invertebrates
organic
particulate
zooplankton
algae
spellingShingle PIE LTER
organic matter
population dynamics
Massachusetts
stable isotope
nitrogen
carbon
food web
trophic
fish
invertebrates
organic
particulate
zooplankton
algae
Stable isotope (carbon and nitrogen) data for functional groups in the Plum Island Sound Estuary.
topic_facet PIE LTER
organic matter
population dynamics
Massachusetts
stable isotope
nitrogen
carbon
food web
trophic
fish
invertebrates
organic
particulate
zooplankton
algae
description Stable isotopes of primary producers will be compared to stable isotopes of functional groups of organisms at primarily three sites within the estuary that have different dominant sources of organic matter. The three sites are: Lower (IBYC, SO-3, mouth of Plum Island Sound, 2-3 km upstream of the mouth of the estuary), Middle (OTL, PR-10.5, upper Sound, lower Parker, 8-11 km upstream of the mouth of the estuary) and Upper (P2, PR-22, upper Parker, above Middle Rd Bridge (22 km upstream of the mouth odf the estuary). The Lower site is dominated by marine phytoplankton, the Middle site is dominated by a mixture of salt marsh and phytoplankton and the Upper site is dominated by oligohaline phytoplankton and fresh marsh. Ten functional groups will be sampled at each site (Surface sediment, benthic diatoms, Nereis, mummichog, ribbed mussels, POM, blue mussels, pelagic copepods (Acartia), silversides and soft shell clams (Mya). Marsh, benthic algae and phytoplankton inputs or benthic vs. pelagic pathways will be evident in the isotopic signals of these functional groups. Samples will be collected between the middle and end of August to reflect a growing season using recently produced OM. Samples of 15 – 20 individuals will be pooled for analysis. Silversides will have 3 different pooled samples for determination of variance.
author2 CharlesHopkinson
HapGarritt
format Dataset
title Stable isotope (carbon and nitrogen) data for functional groups in the Plum Island Sound Estuary.
title_short Stable isotope (carbon and nitrogen) data for functional groups in the Plum Island Sound Estuary.
title_full Stable isotope (carbon and nitrogen) data for functional groups in the Plum Island Sound Estuary.
title_fullStr Stable isotope (carbon and nitrogen) data for functional groups in the Plum Island Sound Estuary.
title_full_unstemmed Stable isotope (carbon and nitrogen) data for functional groups in the Plum Island Sound Estuary.
title_sort stable isotope (carbon and nitrogen) data for functional groups in the plum island sound estuary.
publisher Plum Island Ecosystems LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7485pie_im@mbl.eduhttp://ecosystems.mbl.edu/PIE/
publishDate 2004
url http://hdl.handle.net/10255/dryad.15387
http://metacat.lternet.edu/knb/metacat/knb-lter-pie.13.4/xml
op_coverage P2
P5
Old Town Landing
Nelson Island
IBYC
The Plum Island Ecosystems (PIE) LTER site, is located in northeastern Massachusetts, 42.72 N, 70.85 W. The PIE LTER lies at the interface of a thinly soiled, formerly glaciated New England land mass and the highly productive Gulf of Maine. Three watersheds comprise the estuarine drainage basin: Parker (155 km2), Rowley (26 km2) and Ipswich (404 km2). The Ipswich River watershed is highly urbanized with Boston "bedroom" communities encroaching in the headwater region while the Parker is less urbanized and retains a higher proportion of forest.
-70.91732887 W -70.91732887 E 42.74988851 N 42.74988851 S
-70.87290193 W -70.87290193 E 42.75506932 N 42.75506932 S
-70.8365313 W -70.8365313 E 42.76236849 N 42.76236849 S
-70.8210343 W -70.8210343 E 42.74691643 N 42.74691643 S
-70.79657702 W -70.79657702 E 42.70899476 N 42.70899476 S
-71.2198 W -70.7568 E 42.8276 N 42.4965 S
1999-08-23 to 2008-09-24
genre Nelson Island
Copepods
genre_facet Nelson Island
Copepods
op_relation http://metacat.lternet.edu/knb/metacat/knb-lter-pie.13.4/xml
knb-lter-pie.13.4
http://hdl.handle.net/10255/dryad.15387
op_rights Acceptance and utilization of PIE-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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