Jökull


Jökull - 01.12.2006, Side 31

Jökull - 01.12.2006, Side 31
The stable isotopic (C and N) composition of modern plants and lichens from northern Iceland 0 2 4 6 8-2-4-6-8-10 10-12 0-5-10-15-20-25-30-35-40-45-50 Terrestial C plants (-32 to -20)3 Phytoplankton (-42 to -26) Organic fertilizer (2 to 30) Animal guano (10 to 20) C/N Inorganic fertilizer (-4 to 4) Plants fertilized by animal guanoPlants and lichens receiving N from ammonia Soil (-10 to 15) Precipitation (-15 to 15) Glacier Bay, Alaska -9 to 0.5 Average (3.7± 3.5) TropicalTemperate Average (-2.8±2.0) (-8 to 0.5) (-2 to 6) Methanogenic (-110 to -60) Aquatic macrophytes (-50 to -11) Seagrass (-15 to -3) Terrestial C4 plants ( -17 to -9) Plankton (average -20) CAM plant (-28 to -10) Sediment mixture of aquatic and terrestrial plants (10 to 20) Organic matter in lake composed mainly of terristrial plants (>20)Plankton (~6) Diatoms (5 to 8) 1 4, 8 8, 9,10,11, 3 2 4, 5 7 8 8 8 12 12 12 12 12 12 12 15 14 14 16 16 References References References -9.3 to 1.0 Interior, Alaska Belize Mangroves, central America Upland, United Kingdom 6 12 P limited N limited 160 24 3220 284 8 12 36 40 44 5 A B C 13 Organic matter in lake composed mainly of aquatic plants and lacustrine algae (4 to 10) P la n ts ra n g es d 1 5 N N it r o g en s o u rc e v a lu es d 1 5 N d13C(‰, VPDB) d15N(‰, air) Figure 1. a) Nitrogen isotope variation in ecosystems; b) Carbon isotopic variation in ecosystems; c) C/N vari- ations in ecosystems (An arrow end indicates a range greater than or less than the scale presented while a blunt end indicates the minimum or maximum reported values) (References: 1 Hobbie et al., 1998; 2 Kielland et al., 1998; 3 Martinelli et al., 1999; 4 Erskine et al., 1998; 5 Fogel et al., submitted; 6 McKee et al., 2002; 7 Jones et al., 2004; 8 Kendall, 1998; 9 Garten, 1992; 10 Paerl and Fogel, 1994; 11 Fogg et al., 1998; 12 Boutton, 1991; 13 Keeley and Sandquist, 1992; 14 Herczeg et al., 2001; 15 Meyers, 1994; 16 Lamb et al., 2004). – Yfirlit yfir magn (a) köfnunarefnis (δ15N), (b)kolefnis (δ13C), og (c) hlutföll þeirra (C/N) í mismunandi vistkerfum. JÖKULL No. 56 29
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