| Literature DB >> 27551919 |
Kellie J Carim1, Kyle R Christianson2, Kevin M McKelvey1, William M Pate2, Douglas B Silver2, Brett M Johnson2, Benjamin T Galloway2, Michael K Young1, Michael K Schwartz1.
Abstract
The spread of Mysis diluviana, a small glacial relict crustacean, outside its native range has led to unintended shifts in the composition of native fish communities throughout western North America. As a result, biologists seek accurate methods of determining the presence of M. diluviana, especially at low densities or during the initial stages of an invasion. Environmental DNA (eDNA) provides one solution for detecting M. diluviana, but building eDNA markers that are both sensitive and species-specific is challenging when the distribution and taxonomy of closely related non-target taxa are poorly understood, published genetic data are sparse, and tissue samples are difficult to obtain. To address these issues, we developed a pair of independent eDNA markers to increase the likelihood of a positive detection of M. diluviana when present and reduce the probability of false positive detections from closely related non-target species. Because tissue samples of closely-related and possibly sympatric, non-target taxa could not be obtained, we used synthetic DNA sequences of closely related non-target species to test the specificity of eDNA markers. Both eDNA markers yielded positive detections from five waterbodies where M. diluviana was known to be present, and no detections in five others where this species was thought to be absent. Daytime samples from varying depths in one waterbody occupied by M. diluviana demonstrated that samples near the lake bottom produced 5 to more than 300 times as many eDNA copies as samples taken at other depths, but all samples tested positive regardless of depth.Entities:
Year: 2016 PMID: 27551919 PMCID: PMC4995006 DOI: 10.1371/journal.pone.0161664
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
A list of species and corresponding GenBank accession number for sequences used in marker development.
| Order | Genus | Species | GenBank Accession |
|---|---|---|---|
| Mysidae | AY920494.1, DQ189153.1 -DQ189155.1, EF609241.1—EF609265.1 | ||
| Isopoda | DQ144893.1 | ||
| Cladocera | AY075057.1 | ||
| Cladocera | KC154293.1 | ||
| Amphipoda | JX899356.1 | ||
| Amphipoda | DQ464675.1—DQ464682.1 | ||
| Decapoda | AY701248.1 | ||
| Decapoda | AF474365.1 | ||
| Decapoda | KJ645855.1 |
Primer and probe sequences for the Mysis_A and Mysis_B markers.
| Oligo | Sequence | Final concentration (nM) |
|---|---|---|
| Mysis_A Forward | 5'-CCAGTGTTAGCAGGGGCTAT-3' | 600 |
| Mysis_A Reverse | 5'-CCCACCTACAGGGTCAAAGA-3' | 600 |
| Mysis_A Probe | 5'-TTTAACAGACCGTAATTTAA-3' | 250 |
| Mysis_B Forward | 5'-GAGTTTTAATTCGGTTAGAGTTAGGGC-3' | 900 |
| Mysis_B Reverse | 5'-CATGCGCAGTAACAATTACGTTATAA-3' | 900 |
| Mysis_B Probe | 5'-CATTTGATTGGGGACAGACA-3' | 250 |
Fig 1Map of waterbodies sampled for eDNA detection of M. diluviana in Colorado, USA.
Numbers correspond to Map ID in Table 3.
Summary of sample collection and results.
Year introduced refers to the earliest year of known M. diluviana stocking from Nesler et al. (1986). M. diluviana density (individuals /m2) was estimated using traditional sampling methods. Density estimates were taken within 24 hours of eDNA collection. DNA was quantified using both markers and is listed in copies / L of water sampled.
| Water body | Year introduced | Density (SD) | eDNA collection date | Sample strata (depth in m) | eDNA sampling coordinates | DNA quantity (SD) | ||
|---|---|---|---|---|---|---|---|---|
| Latitude | Longitude | Mysis_A | Mysis_B | |||||
| Dillon Reservoir | 1970 | 171 (62) | 6/18/2014 | Bottom (58) | 39.614399 | -106.061571 | 13358 (959) | 4929 (46) |
| 6/18/2014 | Surface (0) | 39.616058 | -106.061433 | 73 (29) | 15 (10) | |||
| 6/18/2014 | Thermocline (10) | 39.610441 | -106.060858 | 43 (3) | 28 (8) | |||
| 6/18/2014 | Bottom (50) | 39.612698 | -106.056373 | 17410 (407) | 4878 (357) | |||
| 6/18/2014 | Surface (0) | 39.611319 | -106.060417 | 107 (39) | 22 (8) | |||
| 6/18/2014 | Thermocline (10) | 39.616639 | -106.050002 | 58 (69) | 121 (47) | |||
| 7/10/2014 | Bottom (50) | 39.610823 | -106.065302 | 359 (44) | 185 (34) | |||
| 7/10/2014 | Surface (0) | 39.610100 | -106.066619 | 9 (0) | 3 (0) | |||
| 7/10/2014 | Thermocline (10) | 39.600374 | -106.060099 | 68 (43) | 27 (8) | |||
| Lake Granby | 1971 | 294 (94) | 8/13/2015 | Bottom (52) | 40.151051 | -105.865884 | 399 (99) | 272 (16) |
| Jefferson Lake | 1972 | 392 (137) | 8/11/2015 | Bottom (50) | 39.454677 | -105.861831 | 82 (24) | 44 (27) |
| Carter Lake | 1971 | 515 (154) | 10/7/2015 | Bottom (34) | 40.343045 | -105.218825 | 1580 (266) | 1010 (52) |
| Lower Big Creek Lake | 1969 | 3 (3) | 9/10/2015 | Bottom (18) | 40.929748 | -106.608460 | 35 (16) | 25 (6) |
| Stillwater Reservoir | 1974 | 0 | 7/16/2015 | Bottom (14) | 40.025420 | -107.125101 | 0 | 0 |
| Cheesman Reservoir | 1971 | 0 | 6/19/2014 | Bottom (50) | 39.197614 | -105.284399 | 0 | 0 |
| 6/19/2014 | Bottom (49) | 39.202444 | -105.284407 | 0 | 0 | |||
| 6/19/2014 | Bottom (57) | 39.201661 | -105.284207 | 0 | 0 | |||
| Horsetooth Reservoir | 1971 | 0 | 6/3/2016 | Bottom (44) | 40.553807 | -105.149198 | 0 | 0 |
| 6/3/2016 | Bottom (46) | 40.53048 | -105.144293 | 0 | 0 | |||
| Eleven Mile Reservoir | Not stocked | 0 | 7/9/2014 | Bottom (30) | 38.907827 | -105.480703 | 0 | 0 |
| 7/9/2014 | Bottom (30) | 38.907601 | -105.480863 | 0 | 0 | |||
| 7/9/2014 | Bottom (30) | 38.907329 | -105.481277 | 0 | 0 | |||
| Upper Stillwater Reservoir | Not stocked | 0 | 7/15/2015 | Bottom (6) | 40.044299 | -107.074079 | 0 | 0 |