Declining foliar and litter δ15N diverge from soil, epiphyte and input δ15N along a 120000yr temperate rainforest chronosequence

New Phytologist

Volumn 190, Issue 4, 2011, Pages 941-952

  Menge, Duncan N L ^a,b   Troy Baisden, W ^c   Richardson, Sarah J ^d   Peltzer, Duane A ^d   Barbour, Margaret M ^d,e  

^a NATIONAL CENTER FOR ECOLOGICAL ANALYSIS AND SYNTHESIS   (United States)

^b PRINCETON UNIVERSITY   (United States)

^c GNS SCIENCE   (New Zealand)

^d LANDCARE RESEARCH   (New Zealand)

^e UNIVERSITY OF SYDNEY   (Australia)

Author keywords

15N; Ecosystem development; New Zealand; Nitrogen; Stable isotope; Succession; Temperate rainforest

Indexed keywords

NITROGEN;

BRYOPHYTE; CHRONOSEQUENCE; DECOMPOSITION; ENVIRONMENTAL GRADIENT; EPIPHYTE; EVERGREEN TREE; FOLIAGE; LICHEN; LITTER; MYCORRHIZA; NITROGEN ISOTOPE; NUTRIENT UPTAKE; RAINFOREST; SOIL HORIZON; SOIL NITROGEN; STABLE ISOTOPE; SUCCESSION; TEMPERATE FOREST;

ANGIOSPERM; ARTICLE; CHEMISTRY; ECOSYSTEM; LICHENS; METABOLISM; MOSS; NEW ZEALAND; PLANT LEAF; PLANT ROOT; SOIL; TIME; TREE;

ANGIOSPERMS; BRYOPHYTA; ECOSYSTEM; LICHENS; NEW ZEALAND; NITROGEN; NITROGEN ISOTOPES; PLANT LEAVES; PLANT ROOTS; SOIL; TIME FACTORS; TREES;

NEW ZEALAND;

BRYOPHYTA; BRYOPHYTES; CORIARIA ARBOREA; CORIARIACEAE;

EID: 79955780654     PISSN: 0028646X     EISSN: 14698137     Source Type: Journal    
DOI: 10.1111/j.1469-8137.2010.03640.x     Document Type: Article

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