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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Lars G. Rudstam</dc:contributor>
  <dc:contributor>Christopher Hotaling</dc:contributor>
  <dc:contributor>Russ D. McCullough</dc:contributor>
  <dc:contributor>Dave Lemon</dc:contributor>
  <dc:contributor>Web Pearsall</dc:contributor>
  <dc:contributor>Jana Lantry</dc:contributor>
  <dc:contributor>Michael J. Connerton</dc:contributor>
  <dc:contributor>Steve LaPan</dc:contributor>
  <dc:contributor>Zy Biesinger</dc:contributor>
  <dc:contributor>Brian F. Lantry</dc:contributor>
  <dc:contributor>Maureen Walsh</dc:contributor>
  <dc:contributor>Brian Weidel</dc:contributor>
  <dc:creator>Kristen T. Holeck</dc:creator>
  <dc:date>2016</dc:date>
  <dc:description>&lt;ol&gt;&lt;li&gt;Offshore spring total phosphorus (TP) in 2015 was 4.2 μ g/L, the same as in 2014; this is lower than 2001 - 2013, but there is no significant time trend 2001 - 2015. Offshore soluble reactive phosphorus (SRP) was very low in 2015; Apr/May - Oct mean values were &amp;lt;1 μ g/L at most sites. SRP has been stable in nearshore and offshore habitats since 1998 (range, 0.4 – 3.3 μ g/L). TP concentrations were low at both nearshore and offshore locations (range 4.2 - 8.1 μ g/L), and TP and SRP concentrations were significantly higher in the nearshore as compared to the offshore (6.8 μ g/L vs 4.8 μ g/L, TP; 1.1 μ g/L vs 0.7 μ g/L, SRP).&lt;/li&gt;&lt;li&gt;Chlorophyll-&lt;i&gt;a&lt;/i&gt; and Secchi depth values are indicative of oligotrophic conditions in nearshore and offshore habitats. Offshore summer chlorophyll- a declined significantly 2000 - 2015. Nearshore chlorophyll- a increased 1995 - 2004 but then declined 2005 - 2015. Epilimnetic chlorophyll-&lt;i&gt;a&lt;/i&gt; averaged between 0.9 and 1.9 1 μg/L across sites, and offshore concentrations (1.4 1 μg/L) were significantly higher than nearshore (1.1 μg/L). Summer Secchi depth increased significantly in the offshore 2000 -2015 and showed no trend in the nearshore, 1995 - 2015. Apr/May - Oct Secchi depth ranged from 5.0 m to 13.0 m at individual sites and was higher in the offshore (9.5 m) than nearshore (6.2 m).&lt;/li&gt;&lt;li&gt;In 2015, Apr/May - Oct epilimnetic zooplankton density, size, and biomass were not different between the offshore and the nearshore, but cyclopoid biomass was higher in the offshore (8.3 mg/m 3 vs 2.0 mg/m&lt;sup&gt;3&lt;/sup&gt;) and &lt;i&gt;Bythotrephes&lt;/i&gt; biomass was higher in the nearshore (0.17 mg/m&lt;sup&gt;3&lt;/sup&gt; vs 0.04 mg/m&lt;sup&gt;3&lt;/sup&gt;).&lt;/li&gt;&lt;li&gt;Zooplankton density and biomass peaked in September, an atypical pattern. This coincided with peaks in calanoid copepod, daphnid, and &lt;i&gt;Holopedium&lt;/i&gt; &lt;i&gt;Holopedium&lt;/i&gt; biomass in the nearshore has increased significantly since 1995.&lt;/li&gt;&lt;li&gt;The predatory cladoceran &lt;i&gt;Cercopagis&lt;/i&gt; continued to be abundant in summer in the nearshore (3.4 μ g/L) but not in the offshore (0.8 μ g/L). &lt;i&gt;Bythotrephes&lt;/i&gt; biomass was very low (&amp;lt;0.3 μ g/L) in both nearshore and offshore habitats. Combined biomass of these predatory cladocerans in the offshore was the lowest recorded since 2001.&lt;/li&gt;&lt;li&gt;Summer nearshore zooplankton density and biomass declined significantly 1995 - 2004 and then increased significantly 2005 – 2015. The decline was due to reductions in bosminids and cyclopoids and the increase was due mostly to a rebound in bosminids.&lt;/li&gt;&lt;li&gt;Summer offshore zooplankton density and biomass increased significantly 2005 - 2015. The increase was due to an increase in bosminids and cyclopoids. In 2015, offshore summer epilimnetic zooplankton biomass was 52 mg/m&lt;sup&gt;3&lt;/sup&gt; (2005 - 2014 mean=18 mg/m&lt;sup&gt;3&lt;/sup&gt;).&lt;/li&gt;&lt;li&gt;Most zooplankton biomass was found in the metalimnion in July and in the hypolimnion in September. Cyclopoids and &lt;i&gt;Limnocalanus&lt;/i&gt; dominated the metalimnion and &lt;i&gt;Limnocalanus&lt;/i&gt; dominated the hypolimnion. Whole water column samples taken show a stable zooplankton biomass but changing community composition since 2010. Cyclopoids increased 2013 - 2015 and daphnids declined 2014 - 2015.&lt;/li&gt;&lt;/ol&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>New York State Department of Environmental Conservation</dc:publisher>
  <dc:title>2015 status of the Lake Ontario lower trophic levels</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>