Sediment Porosity, Density, %C, %N, and C:N ratios in Waquoit Bay, Massachusetts (USA)

On 7 occasions over the course of 3 years (2011-2013) we conducted hypoxic static core incubations on sediments and water collected in Waquoit Bay Massachusetts (USA) from four stations: Childs River Estuary, Metoxit Point, South Basin, & Sage Lot Pond. The goal of this study was quantify sedime...

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Main Authors: Foster, Sarah, Fulweiler, Robinson W.
Format: Dataset
Language:unknown
Published: figshare 2019
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.7371017
https://figshare.com/articles/Sediment_Porosity_Density_C_N_and_C_N_ratios_in_Waquoit_Bay_Massachusetts_USA_/7371017
id ftdatacite:10.6084/m9.figshare.7371017
record_format openpolar
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
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topic Environmental Chemistry
Oceanography
FOS Earth and related environmental sciences
Geochemistry
spellingShingle Environmental Chemistry
Oceanography
FOS Earth and related environmental sciences
Geochemistry
Foster, Sarah
Fulweiler, Robinson W.
Sediment Porosity, Density, %C, %N, and C:N ratios in Waquoit Bay, Massachusetts (USA)
topic_facet Environmental Chemistry
Oceanography
FOS Earth and related environmental sciences
Geochemistry
description On 7 occasions over the course of 3 years (2011-2013) we conducted hypoxic static core incubations on sediments and water collected in Waquoit Bay Massachusetts (USA) from four stations: Childs River Estuary, Metoxit Point, South Basin, & Sage Lot Pond. The goal of this study was quantify sediment metabolism under water column hypoxia in a shallow, temperate estuarine system. As part of that study we analyzed samples from incubated cores to determine sediment density, porosity, percent carbon (%C), percent nitrogen (%N), and molar carbon to nitrogen (C:N) ratios. These samples were collected using plastic (polycarbonate) syringe sub-cores (60 mL) that we sectioned up to 4 cm in 1 cm sub-samples. We stored the sediments in plastic centrifuge tubes (50 mL) in a freezer until they were analyzed. All sampling materials were acid washed and ethanol rinsed prior to sediment collection. We used standard processing and analysis protocols to determine sediment porosity, density (Nielsen et al. 2000) and %C %N (Zimmermann et al. 1997). Percent C and N samples were determined using an elemental analyzer at the Boston University Stable Isotopes Laboratory. For more information please see articles where these data are published (Foster & Fulweiler 2014, Foster & Fulweiler 2019). Email questions and comments to: sqfoster@bu.edu Sampling Stations CRE = Childs River Estuary (41° 34.805’ N 70°31.826’ W, 1.2 m deep, bottom water salinity 27.3-29.7 psu) MP = Metoxit Point (41° 34.134’ N 70° 31.272’ W, 2.2 m deep, bottom water salinity 29.6-31.3 psu) SB = South Basin (41° 33.404’ N 70° 31.442’ W, 1.8 m deep, bottom water salinity 30.6-31.3 psu)SLP = Sage Lot Pond (41° 33.270’ N 70° 30.584’ W, 1.2 m deep, bottom water salinity 28.9-30.4 psu) Units Depth Range = cmDensity = g/mLPorosity = sediment pore space to total volume ratioCarbon = percent carbon of total massNitrogen = percent nitrogen of total massC:N = carbon to nitrogen molar ratio Abbreviations & Symbols Date = dd (day) - month - yy (year) Stn = Stationm.i. = measurement issuen.m. = not measured Acknowledgments There are numerous people who contributed to this project. We would like to thank the Waquoit Bay National Estuarine Research Reserve (WBNERR) for their continued multi-year support of our research. All sediment samples for this study were collected using WBNERR boats. We are particularly grateful to the following WBNERR employees who assisted with the fieldwork: MK Fox, A Lescher, J Mora, C Weidman. We would also like to thank several Fulweiler Lab members and Boston University Marine Program (BUMP) students for their assistance with fieldwork and sediment sub-coring in the lab: S Andrews, A Banks, S Buckley, K Czapla, S Donovan, D Forest, E Heiss, J Luthringer, M McCarthy, S Newell, MK Rogener, R Schweiker, K Yoshimura. In addition, S Donovan, S Duan, E Greenberg, R Lauto, and D Lewellyn, helped with sediment processing and density/porosity analysis. And R Michener in Boston University’s Stable Isotopes Laboratory analyzed sediment percent carbon and nitrogen. We also thank Boston University Earth and Environment Department for use of their facilities and their general academic and logistical research support. References Foster SQ, and RW Fulweiler. 2019. Estuarine sediments exhibit dynamic and variable biogeochemical responses to hypoxia. Journal of Geophysical Research: Biogeosciences, 124. https://doi.org/10.1029/2018JG004663 Foster SQ and RW Fulweiler. 2014. Spatial and historic variability of benthic nitrogen cycling in an anthropogenically impacted estuary. Frontiers in Marine Science 1. https://doi.org/10.3389/fmars.2014.00056. Nielsen LP, V Brotas, P Viaroli, G Underwood, DB Nedwell, K Sundback, S Rysgaard, et al. 2000. Protocol handbook for NICE - Nitrogen Cycling in Estuaries: A Project under the EU reserach programme: Marine Science and Technology (MAST III). Edited by T Dalsgaard. National Environmental Research Institute, Silkborg, Denmark. Zimmermann CF, CW Keefe, and J Bashe. 1997. Determination of carbon and nitrogen in sediments and particulates of estuarine/coastal waters using elemental analysis. US Environmental Protection Agency, Method 440: 9.
format Dataset
author Foster, Sarah
Fulweiler, Robinson W.
author_facet Foster, Sarah
Fulweiler, Robinson W.
author_sort Foster, Sarah
title Sediment Porosity, Density, %C, %N, and C:N ratios in Waquoit Bay, Massachusetts (USA)
title_short Sediment Porosity, Density, %C, %N, and C:N ratios in Waquoit Bay, Massachusetts (USA)
title_full Sediment Porosity, Density, %C, %N, and C:N ratios in Waquoit Bay, Massachusetts (USA)
title_fullStr Sediment Porosity, Density, %C, %N, and C:N ratios in Waquoit Bay, Massachusetts (USA)
title_full_unstemmed Sediment Porosity, Density, %C, %N, and C:N ratios in Waquoit Bay, Massachusetts (USA)
title_sort sediment porosity, density, %c, %n, and c:n ratios in waquoit bay, massachusetts (usa)
publisher figshare
publishDate 2019
url https://dx.doi.org/10.6084/m9.figshare.7371017
https://figshare.com/articles/Sediment_Porosity_Density_C_N_and_C_N_ratios_in_Waquoit_Bay_Massachusetts_USA_/7371017
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op_doi https://doi.org/10.6084/m9.figshare.7371017
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spelling ftdatacite:10.6084/m9.figshare.7371017 2023-05-15T17:14:17+02:00 Sediment Porosity, Density, %C, %N, and C:N ratios in Waquoit Bay, Massachusetts (USA) Foster, Sarah Fulweiler, Robinson W. 2019 https://dx.doi.org/10.6084/m9.figshare.7371017 https://figshare.com/articles/Sediment_Porosity_Density_C_N_and_C_N_ratios_in_Waquoit_Bay_Massachusetts_USA_/7371017 unknown figshare Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Environmental Chemistry Oceanography FOS Earth and related environmental sciences Geochemistry dataset Dataset 2019 ftdatacite https://doi.org/10.6084/m9.figshare.7371017 2021-11-05T12:55:41Z On 7 occasions over the course of 3 years (2011-2013) we conducted hypoxic static core incubations on sediments and water collected in Waquoit Bay Massachusetts (USA) from four stations: Childs River Estuary, Metoxit Point, South Basin, & Sage Lot Pond. The goal of this study was quantify sediment metabolism under water column hypoxia in a shallow, temperate estuarine system. As part of that study we analyzed samples from incubated cores to determine sediment density, porosity, percent carbon (%C), percent nitrogen (%N), and molar carbon to nitrogen (C:N) ratios. These samples were collected using plastic (polycarbonate) syringe sub-cores (60 mL) that we sectioned up to 4 cm in 1 cm sub-samples. We stored the sediments in plastic centrifuge tubes (50 mL) in a freezer until they were analyzed. All sampling materials were acid washed and ethanol rinsed prior to sediment collection. We used standard processing and analysis protocols to determine sediment porosity, density (Nielsen et al. 2000) and %C %N (Zimmermann et al. 1997). Percent C and N samples were determined using an elemental analyzer at the Boston University Stable Isotopes Laboratory. For more information please see articles where these data are published (Foster & Fulweiler 2014, Foster & Fulweiler 2019). Email questions and comments to: sqfoster@bu.edu Sampling Stations CRE = Childs River Estuary (41° 34.805’ N 70°31.826’ W, 1.2 m deep, bottom water salinity 27.3-29.7 psu) MP = Metoxit Point (41° 34.134’ N 70° 31.272’ W, 2.2 m deep, bottom water salinity 29.6-31.3 psu) SB = South Basin (41° 33.404’ N 70° 31.442’ W, 1.8 m deep, bottom water salinity 30.6-31.3 psu)SLP = Sage Lot Pond (41° 33.270’ N 70° 30.584’ W, 1.2 m deep, bottom water salinity 28.9-30.4 psu) Units Depth Range = cmDensity = g/mLPorosity = sediment pore space to total volume ratioCarbon = percent carbon of total massNitrogen = percent nitrogen of total massC:N = carbon to nitrogen molar ratio Abbreviations & Symbols Date = dd (day) - month - yy (year) Stn = Stationm.i. = measurement issuen.m. = not measured Acknowledgments There are numerous people who contributed to this project. We would like to thank the Waquoit Bay National Estuarine Research Reserve (WBNERR) for their continued multi-year support of our research. All sediment samples for this study were collected using WBNERR boats. We are particularly grateful to the following WBNERR employees who assisted with the fieldwork: MK Fox, A Lescher, J Mora, C Weidman. We would also like to thank several Fulweiler Lab members and Boston University Marine Program (BUMP) students for their assistance with fieldwork and sediment sub-coring in the lab: S Andrews, A Banks, S Buckley, K Czapla, S Donovan, D Forest, E Heiss, J Luthringer, M McCarthy, S Newell, MK Rogener, R Schweiker, K Yoshimura. In addition, S Donovan, S Duan, E Greenberg, R Lauto, and D Lewellyn, helped with sediment processing and density/porosity analysis. And R Michener in Boston University’s Stable Isotopes Laboratory analyzed sediment percent carbon and nitrogen. We also thank Boston University Earth and Environment Department for use of their facilities and their general academic and logistical research support. References Foster SQ, and RW Fulweiler. 2019. Estuarine sediments exhibit dynamic and variable biogeochemical responses to hypoxia. Journal of Geophysical Research: Biogeosciences, 124. https://doi.org/10.1029/2018JG004663 Foster SQ and RW Fulweiler. 2014. Spatial and historic variability of benthic nitrogen cycling in an anthropogenically impacted estuary. Frontiers in Marine Science 1. https://doi.org/10.3389/fmars.2014.00056. Nielsen LP, V Brotas, P Viaroli, G Underwood, DB Nedwell, K Sundback, S Rysgaard, et al. 2000. Protocol handbook for NICE - Nitrogen Cycling in Estuaries: A Project under the EU reserach programme: Marine Science and Technology (MAST III). Edited by T Dalsgaard. National Environmental Research Institute, Silkborg, Denmark. Zimmermann CF, CW Keefe, and J Bashe. 1997. Determination of carbon and nitrogen in sediments and particulates of estuarine/coastal waters using elemental analysis. US Environmental Protection Agency, Method 440: 9. Dataset National Environmental Research Institute DataCite Metadata Store (German National Library of Science and Technology) McCarthy ENVELOPE(66.543,66.543,-70.404,-70.404) Buckley ENVELOPE(163.933,163.933,-84.967,-84.967) Newell ENVELOPE(-59.533,-59.533,-62.333,-62.333) Underwood ENVELOPE(49.350,49.350,-68.133,-68.133)