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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/827298.rdf" xlink:actuate="onRequest">Bulk soil and elemental properties of marsh and infilled pond soils collected in 2014-2015 within Plum Island Ecosystems LTER</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Spivak, A. (2020) Bulk soil and elemental properties of marsh and infilled pond soils collected in 2014-2015 within Plum Island Ecosystems LTER. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2020-11-13 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.827298.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Bulk soil and elemental properties of marsh and infilled pond soils within Plum Island Ecosystems - LTER Dataset Description: &amp;lt;p&amp;gt;Bulk soil and elemental properties of marsh and infilled pond soils within Plum Island Ecosystems - LTER. Bulk soil properties of the soils are complemented with Fourier Transform Infrared Spectroscopy and ramped pyrolysis oxidation measurements of the soils. Data were collected during&amp;amp;nbsp;2014-2015.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Soil cores were collected from three sites within the Plum Island Ecosystems - Long Term Ecological Research (PIE-LTER) domain (MA, USA; 42.74° N, -70.85° W).&amp;amp;nbsp;A core liner was fitted with a gasketed piston and placed on the sediment surface and pushed down into the marsh subsurface, ensuring that the soil column did not compact during collection.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The sites had similar elevations (1.41 - 1.51 m North American Vertical Datum of 1988 [NAVD88]) and salt marsh grass communities, dominated by &amp;lt;em&amp;gt;Spartina patens, S. alterniflora&amp;lt;/em&amp;gt;, and &amp;lt;em&amp;gt;Distichlis spicata&amp;lt;/em&amp;gt;. Permanently inundated ponds within each site had comparable depths (0.24 - 0.30 m) but varied in size (643 - 7,149 m²) and age (40 - 53 years) (Spivak et al., 2017; Spivak et al., 2018).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Soil cores were split lengthwise and sectioned into 1, 2, or 5 cm sections, with higher resolution in the top 30 cm. Soil water content (%) and bulk density (g/cm³) were determined gravimetrically after drying to constant mass (60°C). Samples were sieved (1 mm) to remove root material and homogenized with a Retsch Mixer Mill 200. Soil samples were fumed with hydrochloric acid (Hedges and Stern, 1984) prior to elemental (total organic carbon [TOC]) and isotopic (δ13C) analyses at the Stable Isotope Laboratory in the Marine Biological Laboratory (Woods Hole, MA).&amp;lt;/p&amp;gt;</gco:CharacterString>
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http://lod.bco-dmo.org/id/dataset-parameter/828849.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/828852.rdf
	Name: d13C
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&amp;lt;p&amp;gt;The sites had similar elevations (1.41 - 1.51 m North American Vertical Datum of 1988 [NAVD88]) and salt marsh grass communities, dominated by &amp;lt;em&amp;gt;Spartina patens, S. alterniflora&amp;lt;/em&amp;gt;, and &amp;lt;em&amp;gt;Distichlis spicata&amp;lt;/em&amp;gt;. Permanently inundated ponds within each site had comparable depths (0.24 - 0.30 m) but varied in size (643 - 7,149 m²) and age (40 - 53 years) (Spivak et al., 2017; Spivak et al., 2018).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Soil cores were split lengthwise and sectioned into 1, 2, or 5 cm sections, with higher resolution in the top 30 cm. Soil water content (%) and bulk density (g/cm³) were determined gravimetrically after drying to constant mass (60°C). Samples were sieved (1 mm) to remove root material and homogenized with a Retsch Mixer Mill 200. Soil samples were fumed with hydrochloric acid (Hedges and Stern, 1984) prior to elemental (total organic carbon [TOC]) and isotopic (δ13C) analyses at the Stable Isotope Laboratory in the Marine Biological Laboratory (Woods Hole, MA).&amp;lt;/p&amp;gt;</gco:CharacterString>
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