Table 1 Results from the δ13C, δ15N and 14C analyses on Scutachiltonia axfordi (AM1), Yilgarniella sturtensis (AM2) copepods (cyclopoids and harpacticoids), sediment, roots, particulate organic carbon (POC), dissolved inorganic carbon (DIC) and dissolved organic carbon (DOC).
From: Rainfall as a trigger of ecological cascade effects in an Australian groundwater ecosystem
δ13C | δ15N | LR | HR | |||||||
|---|---|---|---|---|---|---|---|---|---|---|
LR | HR | LR | HR | pMC | Δ14C (‰) | Age (BP) | pMC | Δ14C (‰) | Age (BP) | |
S. axfordi | − 24.14 | − 26.88 ± 0.05 | 10.71 | 8.81 ± 0.09 | 102.84 ± 0.48 | 19.9 ± 4.8 | Modern | 99.86 ± 1.01 | − 9.6 ± 9.9 | Modern |
Y. sturtensis | − 24.55 | − 27.10 | 9.99 | 8.50 | 100.46 ± 0.36 | − 3.7 ± 3.6 | Modern | 100.75 ± 0.81 | − 0.9 ± 8.1 | Modern |
Cycopoida | − 20.45 ± 0.30a | − 21.91 ± 0.30a | 13.90 ± 0.30 | 14.5 ± 0.30 | 100.27 ± 0.56c | − 5.6 ± 5.6c | Modernc | 99.36 ± 0.68c | − 14.7 ± 6.7c | Modernc |
Harpacticoida | − 20.60 ± 0.30a | − 23.50 ± 0.30a | 11.90 ± 0.80 | 15.8 ± 0.80 | ||||||
Roots | − 20.57 ± 0.30a | − 20.90 ± 0.30a | 5.10 ± 2.0 | 12.1 ± 0.30 | 103.63 ± 0.30 | 27.7 ± 3.0 | Modern | 103.34 ± 0.47 | 24.9 ± 4.7 | Modern |
Sediment | − 10.33 ± 0.30a | − 9.65 ± 0.30a | 11.0 ± 1.20 | 11.4 ± 1.20 | 22.16 ± 3.23 | − 780.3 ± 32.1 | 12,100 ± 1170 | 57.68 ± 5.21 | − 428.0 ± 51.7 | 4420 ± 725 |
POC | − 21.58 ± 0.10b | − 26.47 ± 0.10b | 10.73 ± 0.10b | 8.35 ± 0.10b | 86.55 ± 0.76 | − 141.7 ± 7.6 | 1160 ± 70 | 63.86 ± 0.28 | − 366.7 ± 2.8 | 3605 ± 35 |
DOCD13 | − 29.25 ± 0.36 | − 29.35 ± 0.20 | na | na | 91.70 ± 0.46 | − 90.6 ± 4.6 | 695 ± 45 | 92.41 ± 0.62 | − 83.5 ± 6.1 | 630 ± 60 |
DOCW4 | − 31.91 ± 0.50 | − 27.15 ± 0.03 | na | na | 66.76 ± 0.48 | − 337.9 ± 4.8 | 3245 ± 60 | 57.99 ± 0.55 | − 424.9 ± 5.5 | 4380 ± 80 |
DICD13 | − 9.45 ± 0.10b | − 9.39 ± 0.10b | na | na | 82.73 ± 0.30 | − 179.5 ± 3.0 | 1575 ± 30 | 77.90 ± 0.19 | − 227.4 ± 1.9 | 2005 ± 20 |
DICW4 | − 8.75 ± 0.10b | − 8.87 ± 0.10b | na | na | 62.47 ± 0.21 | − 380.5 ± 2.1 | 3835 ± 30 | 59.20 ± 0.17 | − 412.8 ± 1.7 | 4210 ± 25 |