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Elemental concentrations were determined  from single spot ablation in larval shells (85% energy, 10 hz, 200 shots, 25 μm spot diameter) for both larvae and settlers.  Elemental compositions were quantified by external calibration (USGS MACS-3) and internal standardization.  We quantified elemental compositions from count per second (cps) measurements of 24Mg, 55Mn, 59Co, 88Sr, 138Ba, 139La, 208Pb and 46Ca using laser ablation inductively coupled mass spectrometry (213 Nd:YAG laser coupled with Elan DRC II ICPMS) at the University of Massachusetts, Boston (LA-ICPMS).  Elemental abundances were calculated as analyte cps/ 43Ca cps.   We performed a one-point calibration using gas blank and MACS-3, and ran MACS-1 as a check standard every ten samples.  Analytical accuracy and precision based on repeated check standard analyses was 96 + 4.4% (mean + sd).  Each sample was analyzed in triplicate and mean concentrations normalized to calcium are reported. 

Location:
Gulf of Maine: Frenchmen Bay (44 28.239 N -68 15.927 W) to Machais Bay (44 39.350 N -67 21.320 W).</gco:CharacterString>
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&lt;p&gt;Existing larval transport models focus mainly on along-shelf transport and have done little to explicitly incorporate the effects of cross-shelf mixing and transport processes. Yet cross-shelf transits (both outgoing and incoming legs) are critical components of the dispersal paths of coastal invertebrates. This project will explore the role of cross-shelf mixing in the connectivity of blue mussel populations in eastern Maine. Previous work has shown that the Eastern Maine Coastal Current (EMCC) begins to diverge from shore southwest of the Grand Manan Channel and creates a gradient in cross-shelf mixing and larval transport, with cross-shelf mixing being more common on the northeastern end, episodic in the transitional middle area, and then becoming rare in the southwestern half of the region of the Gulf of Maine. As a result, the investigators predict that northeastern populations of mussels are seeded mostly from up-stream sources, while a significant component of self-seeding (local retention) exists in southwestern populations. Larvae settling in the intervening bays are expected to be derived from a mixture of local and up-stream sources. Using a combined empirical and theoretical approach hydrographic, current profile, and larval vertical migration data will be collected and used to develop and validate a high-resolution coastal circulation model coupled to a model of larval behavior. The investigators will model simulations in different years using the empirical data from mussel reproductive output and spawning times. Connectivity predicted from this model will be then tested against independent empirical estimates of connectivity based on trace element fingerprinting for larvae which can be connected to specific natal habitats. Regions of agreement and discrepancy in the model will be identified to guide additional data collection and model refinement. This iterative process will ensure an understanding of both larval transport patterns and processes, and provide estimates of inter-annual variability in connectivity for blue mussel populations in the Gulf of Maine.&lt;/p&gt;</gco:CharacterString>
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&lt;p&gt;The overarching hypothesis of this project is that regional differences in community-level processes are driven by very different patterns of population connectivity and recruitment in a few key species, and that these differences are ultimately caused by regional variation in temperature and food availability and mediated by physical larval transport processes. Hence, the project will test the following hypotheses with manipulative field experiments, field sampling, connectivity estimates, and integrative modeling:&lt;br /&gt;
1) Locally-dispersing species dominate dynamics in regions with a net export of planktonic larvae (Northern GoM), while species with planktonic larvae dominate the dynamics in regions with high settlement and extensive connectivity among populations (Southern GoM).&lt;br /&gt;
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BCO-DMO Data Manager Processing Notes:
* added a conventional header with dataset name, PI name, version date
* modified parameter names to conform with BCO-DMO naming conventions
* replaced character &amp;quot;ﾍ&amp;quot; with an apostrophe in site name &amp;quot;Baileyﾍs Island&amp;quot;
* Removed directionals from decimal degrees (negative longitudes are West; negative latitudes are South)
* Commas in location names changed to semicolons to support export as csv through the JGOFS system. 
* Rounded lat/lons to 5 decimal places from 7.
* After communication with data submitter, Age value &amp;quot;Larval&amp;quot; changed to &amp;quot;Larvae&amp;quot; to be consistent with other values in the Age column.  &amp;quot;Settlers&amp;quot; also changed to &amp;quot;Settler&amp;quot; to match other values of &amp;quot;Settler.&amp;quot;

Data version 2 replaces data version 1:
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* 2017 data submitted as an excel file exported to csv.
* Date format changed to ISO yyyy-mm-dd
* &amp;quot; N&amp;quot; and &amp;quot; W&amp;quot; removed from decimal degrees.  (It is accurately negative for W, positive for N)
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