Larval dispersal drives metapopulation connectivity, a key metric of population resilience to disturbance. Deep-sea larval disperal remains poorly understood due to the limited applicability of nearshore approaches such as larval rearing in-situ. Here, we used laser ablation spectrometry (Jackson School of Geosciences at the University of Texas at Austin) and multivariate statistical analyses (i.e., PERMANOVA and CAP) to quantify larval shell trace elemental fingerprints for deep-sea methane see...
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366 larvae of Gigantidas childressi (urn:lsid:marinespecies.org:taxname:1346725) and Bathymodiolus heckerae (urn:lsid:marinespecies.org:taxname:420693) were collected from eight methane seep sites during the three research cruises using a suction sampler mounted to the Deep Submersible Vehicle (DSV) Alvin (AT- cruises) and the ROV Jason (TN391). Shells were sorted and stored at -20 celsius for 1 year prior to sample preparation. Larval shells were separated into two valves using fine paintbrushes under a dissecting microscope, soaked for 5 minutes in a solution of 15% H2O2 (Suprapur®, Supelco) and 0.05 M NaOH (Suprapur®, Supelco) diluted with Milli-Q® water (EMD Millipore). Valves were then rinsed thoroughly with Milli-Q® water, placed in a drop of 1% HNO3 (Optima® grade, Fisher Scientific) for 5 seconds, and again rinsed with Milli-Q® to remove debris and organic material from valves. Valves were then affixed to microscope slides in random order using double-sided tape. Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) was used to determine larval shell trace elemental composition ("fingerprints") by means of a New Wave 193 nm FX laser ablation system attached to an Agilent 7500ce ICP-MS at the Jackson School of Geosciences at the University of Texas at Austin. Pre-ablation was conducted to remove any surface contaminants (line scan mode; spot size = 35 µm, scan rate = 50 µm/s, repetition rate = 10 Hz; laser fluence = ~1.35 J cm-2). After pre-ablation, samples were ablated within the pre-ablation track (line scan mode; line scan mode; spot size 25 µm; scan rate = 5 µm s-1; repetition rate = 20 Hz; laser fluence = ~1.47 J cm-2) with a sampling depth of 6-7 µm. The concentrations of magnesium (24Mg and 25Mg), calcium (44Ca), chromium (53Cr), manganese (55Mn), iron (57Fe), cobalt (59Co), nickel (60Ni), copper (63Cu), strontium (88Sr), cadmium (111Cd), tin (118Sn), barium (138Ba), and lead (208Pb) were measured. Calcium was used as the internal standard, for which Ca43 was measured and a concentration of 400432 ppm Ca in the shell was assumed (i.e., stoichiometrically pure CaCO3). IOLITE (v.4) trace elemental reduction software was used to convert analyte counts-per-second (CPS) to elemental ratios of calcium (X:CaCO3) and to compute the limits of detection. Samples were bracketed using standard reference materials ECRM-752-NP, NIST 612, and USGS GSE-1G to evaluate instrument precision.
Miller, N., Eggleston, D. B., Arellano, S. M., Young, C. M., He, R., Grace, I. J. (2026). Shell trace elemental data (geochemical fingerprints) from larval samples collected during cruises AT42-24, AT50-04, and TN391 in the Gulf of Mexico and Northwestern Atlantic in 2020, 2021, and 2022. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2026-03-19 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/995312 [access date]
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