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• W2063236591 startingPage "723" @default.
• W2063236591 abstract "Multiple soil resources could limit aboveground net primary production (ANPP) in temperate forests, but most studies have focused on nitrogen (N) availability. We tested a suite of resources including water, multiple measures of N, phosphate (PO4), and extractable ions (calcium (Ca), potassium (K), magnesium (Mg)) as correlates of ANPP across a glacial landform gradient in northwestern Lower Michigan. Our goals were to identify resource correlates of ANPP that could potentially limit productivity, to characterize productivity partitioning to leaves (ANPPL) and wood (ANPPW) across the gradient, and to test soil resource correlates of partitioning. We measured soil resource availability and annual ANPP at 13 sites, and fit models of ANPPW and ANPPL as functions of each resource. We used Akaike's Information Criterion to assess empirical support for models with different functional forms. ANPPW was best correlated with Ca, with a relationship that was asymptotic beyond the four lowest-productivity sites. Both Mg and K covaried with Ca; Mg was also supported as an ANPPW correlate. Soil water and sum of ammonium (NH4) and nitrate (NO3) (ΣN) explained substantial ANPPW variance, but with weaker support than for Ca. ANPPL was best correlated with ΣN; NO3 received support, while Ca received less support but still explained substantial ANPPL variance. These results suggest a potential role for Ca in regulating ANPP, at least in low-productivity sites, while reaffirming the importance of both N and water availability. Partitioning of annual production to ANPPW as a fraction of total ANPP was related to Ca and soil water, but only weakly to ΣN. Production was partitioned equally between ANPPL and ANPPW at low fertility, but ANPPW exceeded ANPPL by 24% at maximum productivity. Given this shift in partitioning, measuring only ANPPW but assuming that ANPPL scales proportionately would overestimate ANPP at higher fertility sites. Although correlative, our results suggest that ANPP is constrained by some combination of N, Ca, and water, and provide motivation for experimental manipulations of these resources to better understand forest responses to human influences. If northern temperate forests are strictly N-limited, as suggested by much of the literature, then anthropogenic N deposition should enhance ANPP. In contrast, if ANPP is limited, or co-limited, by Ca or by soil water, then anthropogenic change (altered precipitation, base cation leaching), could counteract production gains from N deposition." @default.
• W2063236591 created "2016-06-24" @default.
• W2063236591 creator A5034032963 @default.
• W2063236591 creator A5045451408 @default.
• W2063236591 creator A5060279143 @default.
• W2063236591 date "2010-07-01" @default.
• W2063236591 modified "2023-10-16" @default.
• W2063236591 title "Soil calcium, nitrogen, and water are correlated with aboveground net primary production in northern hardwood forests" @default.
• W2063236591 cites W1538806454 @default.
• W2063236591 cites W1549871048 @default.
• W2063236591 cites W1667047485 @default.
• W2063236591 cites W1964545603 @default.
• W2063236591 cites W1965626067 @default.
• W2063236591 cites W1968294805 @default.
• W2063236591 cites W1969577244 @default.
• W2063236591 cites W1974010259 @default.
• W2063236591 cites W1976159068 @default.
• W2063236591 cites W1977401424 @default.
• W2063236591 cites W1980859657 @default.
• W2063236591 cites W1983471118 @default.
• W2063236591 cites W1984683686 @default.
• W2063236591 cites W1985011890 @default.
• W2063236591 cites W1990256974 @default.
• W2063236591 cites W1991029199 @default.
• W2063236591 cites W1992241247 @default.
• W2063236591 cites W1994694982 @default.
• W2063236591 cites W1999629074 @default.
• W2063236591 cites W1999956359 @default.
• W2063236591 cites W2000353463 @default.
• W2063236591 cites W2000602457 @default.
• W2063236591 cites W2000922255 @default.
• W2063236591 cites W2002007452 @default.
• W2063236591 cites W2005377090 @default.
• W2063236591 cites W2006777678 @default.
• W2063236591 cites W2007888787 @default.
• W2063236591 cites W2007956784 @default.
• W2063236591 cites W2008451425 @default.
• W2063236591 cites W2017280273 @default.
• W2063236591 cites W2017627505 @default.
• W2063236591 cites W2020287266 @default.
• W2063236591 cites W2020732234 @default.
• W2063236591 cites W2028035560 @default.
• W2063236591 cites W2031678772 @default.
• W2063236591 cites W2039353427 @default.
• W2063236591 cites W2041274965 @default.
• W2063236591 cites W2042788940 @default.
• W2063236591 cites W2047753483 @default.
• W2063236591 cites W2048741001 @default.
• W2063236591 cites W2048983675 @default.
• W2063236591 cites W2054725516 @default.
• W2063236591 cites W2057759798 @default.
• W2063236591 cites W2061137949 @default.
• W2063236591 cites W2072138155 @default.
• W2063236591 cites W2072926658 @default.
• W2063236591 cites W2073532802 @default.
• W2063236591 cites W2073907608 @default.
• W2063236591 cites W2074772420 @default.
• W2063236591 cites W2075405785 @default.
• W2063236591 cites W2078212268 @default.
• W2063236591 cites W2078423321 @default.
• W2063236591 cites W2081963950 @default.
• W2063236591 cites W2082646383 @default.
• W2063236591 cites W2084664377 @default.
• W2063236591 cites W2088245366 @default.
• W2063236591 cites W2096398558 @default.
• W2063236591 cites W2098776234 @default.
• W2063236591 cites W2100544654 @default.
• W2063236591 cites W2101426854 @default.
• W2063236591 cites W2103302046 @default.
• W2063236591 cites W2114878127 @default.
• W2063236591 cites W2116279112 @default.
• W2063236591 cites W2117559600 @default.
• W2063236591 cites W2117581799 @default.
• W2063236591 cites W2121213482 @default.
• W2063236591 cites W2122681058 @default.
• W2063236591 cites W2126855816 @default.
• W2063236591 cites W2136837475 @default.
• W2063236591 cites W2137946753 @default.
• W2063236591 cites W2138258560 @default.
• W2063236591 cites W2138452721 @default.
• W2063236591 cites W2138925628 @default.
• W2063236591 cites W2143322314 @default.
• W2063236591 cites W2143373734 @default.
• W2063236591 cites W2154028481 @default.
• W2063236591 cites W2158009744 @default.
• W2063236591 cites W2165336309 @default.
• W2063236591 cites W2165661110 @default.
• W2063236591 cites W2168983481 @default.
• W2063236591 cites W2169271265 @default.
• W2063236591 cites W2169651581 @default.
• W2063236591 cites W2170743438 @default.
• W2063236591 cites W2173155723 @default.
• W2063236591 cites W2314732280 @default.
• W2063236591 cites W2325733876 @default.
• W2063236591 cites W285115924 @default.
• W2063236591 cites W4238342331 @default.
• W2063236591 cites W4251314665 @default.
• W2063236591 doi "https://doi.org/10.1016/j.foreco.2010.05.029" @default.

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