Table 2:
system | site code |
sample year |
Fundulus heteroclitus | Menidia menidia | Data Source |
|||||
---|---|---|---|---|---|---|---|---|---|---|
mean ± st. dev. MeHg (ng/g DW) |
range MeHg (ng/g DW) |
n | mean ± st. dev. MeHg LNST (ng/g DW) |
mean ± st. dev. THg (ng/g DW) |
range THg (ng/g DW) |
n | ||||
Berry's Creek | 3A | 2016 | 658 ± 192 | 502-931 | 5 | 437 ± 159 | 1380 ± 384 | 1032-1982 | 5 | |
Berry's Creek | EU | 2016 | 830 ± 498 | 332-1465 | 5 | 534 ± 286 | ||||
Berry's Creek | ST | 2016 | 851 ± 284 | 565-1237 | 5 | 478 ± 188 | ||||
Chesapeake | JP-H | 2013 | 26 ± 23 | 7-118 | 27 | 26 ± 15 | 48 ± 48 | 23-166 | 8 | Taylor et al., 2019 |
Chesapeake | JP-L | 2013 | 31 ± 9 | 13-50 | 19 | 26 ± 9 | 48 ± 25 | 15-90 | 12 | Taylor et al., 2019 |
Chesapeake | PC-H | 2013 | 18 ± 4 | 11-24 | 5 | 15 ± 3 | 28 ± 19 | 15-76 | 17 | Taylor et al., 2019 |
Chesapeake | PC-L | 2013 | 27 ± 5 | 23-31 | 4 | 23 ± 4 | 33 ± 10 | 24-49 | 5 | Taylor et al., 2019 |
Delaware River | BW | 2012 | 61 ± 16 | 47-83 | 4 | 49 ± 15 | Buckman et al., 2017 | |||
Delaware River | FS | 2012 | 44 ± 13 | 20-61 | 12 | 46 ± 10 | 77 ± 21 | 59-107 | 4 | Buckman et al., 2017 |
Delaware River | GC | 2012 | 50 ± 8 | 41-57 | 3 | 87 ± 11 | Buckman et al., 2017 | |||
Delaware River | LM | 2012 | 123 ± 57 | 83-245 | 7 | 117 ± 50 | Buckman et al., 2017 | |||
Delaware River | NB | 2012 | 89 ± 141 | 19-489 | 10 | 87 ± 115 | 59 ± 2 | 58-61 | 3 | Buckman et al., 2017 |
Delaware River | PL | 2012 | 91 ± 23 | 59-128 | 6 | 85 ± 17 | 64 ± 15 | 54-82 | 3 | Buckman et al., 2017 |
Delaware River | PT | 2012 | 121 ± 59 | 68-208 | 5 | 105 ± 37 | Buckman et al., 2017 | |||
Delaware River | SB | 2012 | 48 ± 28 | 18-88 | 7 | 59 ± 38 | 69 ± 8 | 60-77 | 3 | Buckman et al., 2017 |
Delaware River | SB-H | 2015 | 103 ± 35 | 76-162 | 5 | 107 ± 46 | 101 ± 20 | 82-133 | 5 | |
Delaware River | SB-L | 2015 | 100 ± 26 | 72-129 | 5 | |||||
Delaware River | SL | 2012 | 130 ± 57 | 57-261 | 14 | 133 ± 56 | Buckman et al., 2017 | |||
Delaware River | TB | 2012 | 59 ± 21 | 13-89 | 9 | 56 ± 21 | Buckman et al., 2017 | |||
Delaware River | WB-H | 2015 | 111 ± 30 | 81-156 | 5 | 111 ± 30 | 72 ± 15 | 60-90 | 5 | |
Delaware River | WB-L | 2015 | 153 ± 49 | 95-217 | 5 | 157 ± 47 | 85 ± 7 | 73-91 | 5 | |
Hackensack River | LH | 2016 | 410 ± 86 | 276-492 | 5 | 297 ± 87 | 267 ± 146 | 188-529 | 5 | |
Hackensack River | RP | 2016 | 317 ± 49 | 270-390 | 5 | 265 ± 32 | 858 ± 269 | 538-1140 | 5 | |
Hackensack River | VP | 2016 | 126 ± 42 | 89-188 | 5 | |||||
Long Island Sound | BI-H | 2013 | 42 ± 15 | 29-66 | 5 | 55 ± 19 | 169 ± 19 | 153-190 | 5 | Taylor et al., 2019 |
Long Island Sound | BI-H | 2015 | 50 ± 26 | 24-85 | 5 | 48 ± 26 | 157 ± 58 | 84-241 | 5 | |
Long Island Sound | BI-L | 2013 | 179 ± 44 | 119-241 | 5 | Taylor et al., 2019 | ||||
Long Island Sound | BI-L | 2015 | 130 ± 34 | 82-161 | 5 | 122 ± 24 | 185 ± 22 | 164-217 | 5 | |
Long Island Sound | GC-H | 2013 | 14 ± 6 | 8-21 | 5 | 17 ± 5 | 70 ± 11 | 50-80 | 5 | Taylor et al., 2019 |
Long Island Sound | GC-H | 2015 | 46 ± 11 | 35-64 | 5 | 45 ± 7 | 99 ± 24 | 66-130 | 5 | |
Long Island Sound | GC-L | 2013 | 14 | 1 | 33 | 103 ± 34 | 79-163 | 5 | Taylor et al., 2019 | |
Mt. Desert Island | BH-H | 2013 | 63 ± 33 | 23-166 | 40 | 67 ± 31 | 189 ± 49 | 110-269 | 15 | Taylor et al., 2019 |
Mt. Desert Island | BH-L | 2013 | 84 ± 24 | 55-148 | 12 | 106 ± 37 | 118 ± 34 | 60-217 | 23 | Taylor et al., 2019 |
Mt. Desert Island | NEC-H | 2013 | 111 ± 28 | 80-137 | 5 | 122 ± 33 | Taylor et al., 2019 | |||
Mt. Desert Island | NEC-L | 2013 | 81 ± 62 | 21-167 | 5 | 83 ± 64 | 104 ± 27 | 78-149 | 5 | Taylor et al., 2019 |
Penobscot River | O | 2016 | 433 ± 116 | 304-575 | 5 | 475 ± 117 | ||||
Penobscot River | V | 2016 | 338 ± 112 | 241-518 | 5 | 357 ± 110 | ||||
Webhannet River | DI-H | 2015 | 30 ± 9 | 18-40 | 5 | 30 ± 9 | 34 ± 4 | 28-39 | 5 | |
Webhannet River | DI-L | 2015 | 19 ± 9 | 7-31 | 5 | 18 ± 9 | 41 ± 5 | 38-48 | 5 | |
Webhannet River | SM-H | 2015 | 25 ± 7 | 19-37 | 5 | 25 ± 7 | 45 ± 5 | 41-54 | 5 | |
Webhannet River | SM-L | 2015 | 52 ± 26 | 13-73 | 5 | 52 ± 26 | 57 ± 16 | 42-82 | 5 |