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DE Nitrogen; Net N mineralization; Oligotrophication; Natural abundance
foliar N isotopes; Northern hardwood forest
ID FREEZE-THAW CYCLES; NATURAL-ABUNDANCE; CLIMATE-CHANGE; MICROBIAL
BIOMASS; FUTURE CHANGES; NEW-HAMPSHIRE; METAANALYSIS; N-15;
NORTHEASTERN; NITRATE
That's what Zotero uses for keywords and it does get them for me.
FN Clarivate Analytics Web of Science
VR 1.0
PT J
AU Harrison, Jamie L.
Schultz, Kyle
Blagden, Megan
Sanders-DeMott, Rebecca
Templer, Pamela H.
TI Growing season soil warming may counteract trend of nitrogen
oligotrophication in a northern hardwood forest
SO BIOGEOCHEMISTRY
VL 151
IS 2-3
BP 139
EP 152
DI 10.1007/s10533-020-00717-z
EA OCT 2020
PD DEC 2020
PY 2020
AB Over the next century, many mid and high latitude temperate ecosystems
are projected to experience rising growing season temperatures and
increased frequency of soil freeze/thaw cycles (FTCs) due to a reduction
in the depth and duration of the winter snowpack. We conducted a
manipulative field experiment in a northern hardwood forest at the
Hubbard Brook Experimental Forest in New Hampshire to determine the
interactive effects of climate change across seasons on rates of net N
mineralization, foliar N, and natural abundance foliar N-15 (delta N-15)
in red maple (Acer rubrum) trees. We warmed soils 5 degrees C above
ambient temperatures and induced winter FTCs to simulate projected
changes over the next century. Net N mineralization was dominated by
ammonification and increased with warmer soil temperatures, but was not
affected by soil FTCs in the previous winter. Similarly, warming led to
increased foliar N concentrations and delta N-15, with no effect of soil
FTCs. Together, our results show that growing season soil warming
increases soil N availability and N uptake by trees, which may offset
the previously observed negative effects of a smaller snowpack and more
frequent soil freezing on N cycling. We conclude that soil warming in
the growing season may counteract the trend of reduced soil N
availability relative to plant N demand (i.e. N oligotrophication)
observed in northern hardwood forests. This research demonstrates that
climate change across seasons affects N cycling in northern hardwood
forests in ways that would have not been apparent from examining one
season alone.
OI Harrison, Jamie/0000-0001-7937-0503
ZB 0
ZR 0
ZA 0
TC 0
ZS 0
Z8 0
Z9 0
SN 0168-2563
EI 1573-515X
UT WOS:000585767800001
ER
EF
FN Clarivate Analytics Web of Science
VR 1.0
PT J
AU Harrison, JL
Schultz, K
Blagden, M
Sanders-DeMott, R
Templer, PH
AF Harrison, Jamie L.
Schultz, Kyle
Blagden, Megan
Sanders-DeMott, Rebecca
Templer, Pamela H.
TI Growing season soil warming may counteract trend of nitrogen
oligotrophication in a northern hardwood forest
SO BIOGEOCHEMISTRY
DT Article
DE Nitrogen; Net N mineralization; Oligotrophication; Natural abundance
foliar N isotopes; Northern hardwood forest
ID FREEZE-THAW CYCLES; NATURAL-ABUNDANCE; CLIMATE-CHANGE; MICROBIAL
BIOMASS; FUTURE CHANGES; NEW-HAMPSHIRE; METAANALYSIS; N-15;
NORTHEASTERN; NITRATE
AB Over the next century, many mid and high latitude temperate ecosystems are projected to experience rising growing season temperatures and increased frequency of soil freeze/thaw cycles (FTCs) due to a reduction in the depth and duration of the winter snowpack. We conducted a manipulative field experiment in a northern hardwood forest at the Hubbard Brook Experimental Forest in New Hampshire to determine the interactive effects of climate change across seasons on rates of net N mineralization, foliar N, and natural abundance foliar N-15 (delta N-15) in red maple (Acer rubrum) trees. We warmed soils 5 degrees C above ambient temperatures and induced winter FTCs to simulate projected changes over the next century. Net N mineralization was dominated by ammonification and increased with warmer soil temperatures, but was not affected by soil FTCs in the previous winter. Similarly, warming led to increased foliar N concentrations and delta N-15, with no effect of soil FTCs. Together, our results show that growing season soil warming increases soil N availability and N uptake by trees, which may offset the previously observed negative effects of a smaller snowpack and more frequent soil freezing on N cycling. We conclude that soil warming in the growing season may counteract the trend of reduced soil N availability relative to plant N demand (i.e. N oligotrophication) observed in northern hardwood forests. This research demonstrates that climate change across seasons affects N cycling in northern hardwood forests in ways that would have not been apparent from examining one season alone.
OI Harrison, Jamie/0000-0001-7937-0503
FU NSF Long Term Ecological Research (LTER) Grant (NSF)National Science
Foundation (NSF) [1114804, 1637685]; NSF CAREER grant (NSF) [DEB1149929]
FX This research was supported by an NSF Long Term Ecological Research
(LTER) Grant to Hubbard Brook (NSF 1114804 and 1637685) and an NSF
CAREER grant to PHT (NSF DEB1149929).
NR 64
TC 0
Z9 0
SN 0168-2563
EI 1573-515X
PD DEC
PY 2020
VL 151
IS 2-3
BP 139
EP 152
DI 10.1007/s10533-020-00717-z
EA OCT 2020
WC Environmental Sciences; Geosciences, Multidisciplinary
SC Environmental Sciences & Ecology; Geology
DA 2021-02-11
ER
EF
Zotero just uses that file, so without the keywords in there, there's no way they'd import.