#PAGE_PARAMS# #ADS_HEAD_SCRIPTS# #MICRODATA#

Determinants of temperature sensitivity of soil respiration with the decline of a foundation species


Autoři: Danielle D. Ignace aff001
Působiště autorů: Department of Biological Sciences, Smith College, Northampton, MA, United States of America aff001
Vyšlo v časopise: PLoS ONE 14(10)
Kategorie: Research Article
prolekare.web.journal.doi_sk: https://doi.org/10.1371/journal.pone.0223566

Souhrn

The eastern hemlock (Tsuga canadensis) is an important foundation species that is currently declining throughout eastern U.S. forests due to the exotic pests hemlock woolly adelgid (Adelges tsugae) and elongate hemlock scale (Fiorinia externa). Hemlock is often replaced by deciduous tree species, such as black birch (Betula lenta), and has been shown to have large consequences for carbon dynamics due to a substantial loss of soil organic layer carbon storage in hemlock forests when replaced by birch and higher decomposition found in black birch stands. Soil carbon is one of the most important components of the global carbon cycle and has high potential to feedback to climate change when large portions of stored carbon are lost to the atmosphere. There is a general consensus that soil respiration increases with temperature, but there has yet to be a consensus on how temperature sensitivity of soil respiration is affected by various biotic and abiotic factors, such as soil moisture and substrate quality. In this study, the effects of soil temperature and soil moisture on soil respiration (Rs), the temperature sensitivity of soil respiration (Q10), and soil basal respiration (R10) were investigated for hemlock, young birch, and mature birch forest types annually for three years. The Rs values of the three forest types were primarily driven by soil temperature rather than by soil moisture across all years. Soil respiration data collected from hemlock, young birch, and mature birch stands were used to determine annual Q10 and R10 values. The Q10 and R10 values were not significantly different between forest stands, but they were significantly different over the three years. Determinants of Q10 and R10 differed between forest type, with soil moisture primarily influencing Q10 in hemlock and mature birch stands and soil temperature primarily influencing R10 in mature birch stands. The results suggest a complex interaction of soil moisture and soil temperature, and potentially substrate quality and quantity, as determinants of temperature sensitivities in eastern U.S. forests that have transitioned from hemlock-dominated to black birch-dominated forests.

Klíčová slova:

Ecosystems – Forests – Forest ecology – Trees – Carbon dioxide – Soil respiration – Q10 temperature coefficient – Birches


Zdroje

1. IPCC. Summary for Policymakers By: Field, Christopher B.; Barros, Vicente R.; Mastrandrea, Michael D.; et al. Edited by: Field CB; Barros VR; Dokken DJ; et al. CLIMATE CHANGE 2014: IMPACTS, ADAPTATION, AND VULNERABILITY, PT A: GLOBAL AND SECTORAL ASPECTS: WORKING GROUP II CONTRIBUTION TO THE FIFTH ASSESSMENT REPORT OF THE INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE. Cambridge Univ Press; 2014.

2. Schlesinger WH, Andrews JA. Soil respiration and the global carbon cycle. Biogeochemistry. 2000;48: 7–20. doi: 10.1023/A:1006247623877

3. Hashimoto S, Carvalhais N, Ito A, Migliavacca M, Nishina K, Reichstein M. Global spatiotemporal distribution of soil respiration modeled using a global database. Biogeosciences. 2015;12: 4121–4132. doi: 10.5194/bg-12-4121-2015

4. Hursh A, Ballantyne A, Cooper L, Maneta M, Kimball J, Watts J. The sensitivity of soil respiration to soil temperature, moisture, and carbon supply at the global scale. Glob Change Biol. 2017;23: 2090–2103. doi: 10.1111/gcb.13489 27594213

5. Bond-Lamberty B, Thomson A. Temperature-associated increases in the global soil respiration record. Nature. 2010;464: 579–U132. doi: 10.1038/nature08930 20336143

6. Bond-Lamberty B, Thomson A. A global database of soil respiration data. Biogeosciences. 2010;7: 1915–1926. doi: 10.5194/bg-7-1915-2010

7. Ballantyne AP, Andres R, Houghton R, Stocker BD, Wanninkhof R, Anderegg W, et al. Audit of the global carbon budget: estimate errors and their impact on uptake uncertainty. Biogeosciences. 2015;12: 2565–2584. doi: 10.5194/bg-12-2565-2015

8. Bond-Lamberty B, Bailey VL, Chen M, Gough CM, Vargas R. Globally rising soil heterotrophic respiration over recent decades. Nature. 2018;560: 80–83. doi: 10.1038/s41586-018-0358-x 30068952

9. Carey JC, Tang J, Templer PH, Kroeger KD, Crowther TW, Burton AJ, et al. Temperature response of soil respiration largely unaltered with experimental warming. Proc Natl Acad Sci U S A. 2016;113: 13797–13802. doi: 10.1073/pnas.1605365113 27849609

10. Davidson EA, Richardson AD, Savage KE, Hollinger DY. A distinct seasonal pattern of the ratio of soil respiration to total ecosystem respiration in a spruce-dominated forest. Glob Change Biol. 2006;12: 230–239. doi: 10.1111/j.1365-2486.2005.01062.x

11. Davidson EA, Janssens IA. Temperature sensitivity of soil carbon decomposition and feedbacks to climate change. Nature. 2006;440: 165–173. doi: 10.1038/nature04514 16525463

12. Kirschbaum MUF. Will changes in soil organic carbon act as a positive or negative feedback on global warming? Biogeochemistry. 2000;48: 21–51. doi: 10.1023/A:1006238902976

13. Snyder CD, Young JA, Lemarie DP, Smith DR. Influence of eastern hemlock (Tsuga canadensis) forests on aquatic invertebrate assemblages in headwater streams. Can J Fish Aquat Sci. 2002;59: 262–275. doi: 10.1139/F02-003

14. Hadley JL, Schedlbauer JL. Carbon exchange of an old-growth eastern hemlock (Tsuga canadensis) forest in central New England. Tree Physiol. 2002;22: 1079–1092. doi: 10.1093/treephys/22.15-16.1079 12414368

15. Tingley MW, Orwig DA, Field R, Motzkin G. Avian response to removal of a forest dominant: consequences of hemlock woolly adelgid infestations. J Biogeogr. 2002;29: 1505–1516. doi: 10.1046/j.1365-2699.2002.00789.x

16. Ellison AM, Bank MS, Clinton BD, Colburn EA, Elliott K, Ford CR, et al. Loss of foundation species: consequences for the structure and dynamics of forested ecosystems. Front Ecol Environ. 2005;3: 479–486. doi: 10.1890/1540-9295(2005)003[0479:LOFSCF]2.0.CO;2

17. Lovett GM, Canham CD, Arthur MA, Weathers KC, Fitzhugh RD. Forest ecosystem responses to exotic pests and pathogens in eastern North America. Bioscience. 2006;56: 395–405. doi: 10.1641/0006-3568(2006)056[0395:FERTEP]2.0.CO;2

18. Zukswert JM, Bellemare J, Rhodes AL, Sweezy T, Gallogly M, Acevedo S, et al. Forest Community Structure Differs, but Not Ecosystem Processes, 25 Years After Eastern Hemlock Removal in an Accidental Experiment. Southeastern Naturalist. 2014;13: 61–87. doi: 10.1656/058.013.s615

19. Siddig AAH, Ellison AM, Mathewson BG. Assessing the impacts of the decline of Tsuga canadensis stands on two amphibian species in a New England forest. Ecosphere. 2016;7: e01574. doi: 10.1002/ecs2.1574

20. Ignace DD, Fassler A, Bellemare J. Decline of a foundation tree species due to invasive insects will trigger net release of soil organic carbon. Ecosphere. 2018;9: e02391. doi: 10.1002/ecs2.2391

21. Orwig DA, Plotkin AAB, Davidson EA, Lux H, Savage KE, Ellison AM. Foundation species loss affects vegetation structure more than ecosystem function in a northeastern USA forest. PeerJ. 2013;1: e41. doi: 10.7717/peerj.41 23638378

22. Finzi AC, Raymer PCL, Giasson M-A, Orwig DA. Net primary production and soil respiration in New England hemlock forests affected by the hemlock woolly adelgid. Ecosphere. 2014;5: 98. doi: 10.1890/ES14-00102.1

23. Jenkins JC, Aber JD, Canham CD. Hemlock woolly adelgid impacts on community structure and N cycling rates in eastern hemlock forests. Can J For Res-Rev Can Rech For. 1999;29: 630–645. doi: 10.1139/cjfr-29-5-630

24. Orwig DA, Foster DR, Mausel DL. Landscape patterns of hemlock decline in New England due to the introduced hemlock woolly adelgid. J Biogeogr. 2002;29: 1475–1487. doi: 10.1046/j.1365-2699.2002.00765.x

25. Cobb RC. Species shift drives decomposition rates following invasion by hemlock woolly adelgid. Oikos. 2010;119: 1291–1298. doi: 10.1111/j.1600-0706.2009.18308.x

26. Gritsch C, Zimmermann M, Zechmeister-Boltenstern S. Interdependencies between temperature and moisture sensitivities of CO2 emissions in European land ecosystems. Biogeosciences. 2015;12: 5981–5993. https://doi.org/10.5194/bg-12-5981-2015

27. Hamdi S, Moyano F, Sall S, Bernoux M, Chevallier T. Synthesis analysis of the temperature sensitivity of soil respiration from laboratory studies in relation to incubation methods and soil conditions. Soil Biology and Biochemistry. 2013;58: 115–126. doi: 10.1016/j.soilbio.2012.11.012

28. Lovett GM, Weathers KC, Arthur MA, Schultz JC. Nitrogen cycling in a northern hardwood forest: Do species matter? Biogeochemistry. 2004;67: 289–308. doi: 10.1023/B:BIOG.0000015786.65466.f5

29. Humphreys ER, Andrew Black T, Morgenstern K, Li Z, Nesic Z. Net ecosystem production of a Douglas-fir stand for 3 years following clearcut harvesting. Glob Change Biol. 2005;11: 450–464. doi: 10.1111/j.1365-2486.2005.00914.x

30. R Core Team. R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. URL https://www.R-project.org/. 2017.

31. Raich JW, Potter CS, Bhagawati D. Interannual variability in global soil respiration, 1980–94. Global Change Biology. 2002;8: 800–812. doi: 10.1046/j.1365-2486.2002.00511.x

32. Raymer PCL, Orwig DA, Finzi AC. Hemlock loss due to the hemlock woolly adelgid does not affect ecosystem C storage but alters its distribution. Ecosphere. 2013;4: UNSP 63. doi: 10.1890/ES12-00362.1

33. Giasson M-A, Ellison AM, Bowden RD, Crill PM, Davidson EA, Drake JE, et al. Soil respiration in a northeastern US temperate forest: a 22-year synthesis. Ecosphere. 2013;4: UNSP 140. doi: 10.1890/ES13.00183.1

34. Drake JE, Giasson M-A, Spiller KJ, Finzi AC. Seasonal plasticity in the temperature sensitivity of microbial activity in three temperate forest soils. Ecosphere. 2013;4: UNSP 77. doi: 10.1890/ES13-00020.1

35. Craine JM, Fierer N, McLauchlan KK. Widespread coupling between the rate and temperature sensitivity of organic matter decay. Nature Geoscience. 2010;3: 854–857. doi: 10.1038/ngeo1009

36. Fang C, Smith P, Moncrieff JB, Smith JU. Similar response of labile and resistant soil organic matter pools to changes in temperature. Nature. 2005;433: 57–59. doi: 10.1038/nature03138 15635408

37. Conen F, Leifeld J, Seth B, Alewell C. Warming mineralises young and old soil carbon equally. Biogeosciences. 2006;3: 515–519. https://doi.org/10.5194/bg-3-515-2006

38. Lefèvre R, Barré P, Moyano FE, Christensen BT, Bardoux G, Eglin T, et al. Higher temperature sensitivity for stable than for labile soil organic carbon—evidence from incubations of long-term bare fallow soils. Glob Chang Biol. 2014;20: 633–640. doi: 10.1111/gcb.12402 24115336

39. Conant RT, Steinweg JM, Haddix ML, Paul EA, Plante AF, Six J. Experimental warming shows that decomposition temperature sensitivity increases with soil organic matter recalcitrance. Ecology. 2008;89: 2384–2391. doi: 10.1890/08-0137.1 18831158

40. Hartley IP, Ineson P. Substrate quality and the temperature sensitivity of soil organic matter decomposition. Soil Biol Biochem. 2008;40: 1567–1574. doi: 10.1016/j.soilbio.2008.01.007

41. von Luetzow M, Koegel-Knabner I. Temperature sensitivity of soil organic matter decomposition-what do we know? Biol Fertil Soils. 2009;46: 1–15. doi: 10.1007/s00374-009-0413-8

42. Conant RT, Ryan MG, Ågren GI, Birge HE, Davidson EA, Eliasson PE, et al. Temperature and soil organic matter decomposition rates–synthesis of current knowledge and a way forward. Global Change Biology. 2011;17: 3392–3404. doi: 10.1111/j.1365-2486.2011.02496.x

43. Gershenson A, Bader NE, Cheng W. Effects of substrate availability on the temperature sensitivity of soil organic matter decomposition. Glob Change Biol. 2009;15: 176–183. doi: 10.1111/j.1365-2486.2008.01827.x

44. Fassler A, Bellemare J, Ignace DD. Loss of a Foundation Species, Eastern Hemlock (Tsuga canadensis), May Lead to Biotic Homogenization of Fungal Communities and Altered Bacterial Abundance in the Forest Floor. nena. 2019;26: 684–712. doi: 10.1656/045.026.0322

45. Bosatta E, Ågren GI. Soil organic matter quality interpreted thermodynamically. Soil Biology and Biochemistry. 1999;31: 1889–1891. doi: 10.1016/S0038-0717(99)00105-4

46. Eastwood DC, Floudas D, Binder M, Majcherczyk A, Schneider P, Aerts A, et al. The Plant Cell Wall-Decomposing Machinery Underlies the Functional Diversity of Forest Fungi. Science. 2011;333: 762–765. doi: 10.1126/science.1205411 21764756

47. Hibbett DS, Donoghue MJ. Analysis of character correlations among wood decay mechanisms, mating systems, and substrate ranges in homobasidiomycetes. Systematic biology. 2001;50: 215–242. doi: 10.1080/10635150121079 12116929

48. Ishida TA, Nara K, Hogetsu T. Host effects on ectomycorrhizal fungal communities: insight from eight host species in mixed conifer-broadleaf forests. New Phytol. 2007;174: 430–440. doi: 10.1111/j.1469-8137.2007.02016.x 17388905

49. Tyler G. Tree species affinity of decomposer and ectomycorrhizal macrofungi in beech (Fagus sylvatica L.), oak (Quercus robur L.) and hornbeam (Carpinus betulus L.) forests. Forest Ecology and Management. 1992;47: 269–284. doi: 10.1016/0378-1127(92)90279-I

50. Smith ME, Douhan GW, Fremier AK, Rizzo DM. Are true multihost fungi the exception or the rule? Dominant ectomycorrhizal fungi on Pinus sabiniana differ from those on co-occurring Quercus species. The New phytologist. 2009;182: 295–299. doi: 10.1111/j.1469-8137.2009.02801.x 19302178

51. Finzi AC, Van Breemen N, Canham CD. Canopy tree soil interactions within temperate forests: Species effects on soil carbon and nitrogen. Ecol Appl. 1998;8: 440–446. doi: 10.2307/2641083

52. Finzi AC, Canham CD, Van Breemen N. Canopy tree soil interactions within temperate forests: Species effects on pH and cations. Ecol Appl. 1998;8: 447–454. doi: 10.2307/2641084

53. Kizlinski ML, Orwig DA, Cobb RC, Foster DR. Direct and indirect ecosystem consequences of an invasive pest on forests dominated by eastern hemlock. J Biogeogr. 2002;29: 1489–1503. doi: 10.1046/j.1365-2699.2002.00766.x

54. Blagodatskaya EV, Anderson TH. Interactive effects of pH and substrate quality on the fungal-to-bacterial ratio and QCO(2) of microbial communities in forest soils. Soil Biol Biochem. 1998;30: 1269–1274. doi: 10.1016/S0038-0717(98)00050-9

55. Fierer N, Jackson RB. The diversity and biogeography of soil bacterial communities. Proc Natl Acad Sci USA. 2006;103: 626–631. doi: 10.1073/pnas.0507535103 16407148

56. Davidson EA, Belk E, Boone RD. Soil water content and temperature as independent or confounded factors controlling soil respiration in a temperate mixed hardwood forest. Global Change Biology. 4: 217–227. doi: 10.1046/j.1365-2486.1998.00128.x


Článok vyšiel v časopise

PLOS One


2019 Číslo 10
Najčítanejšie tento týždeň
Najčítanejšie v tomto čísle
Kurzy

Zvýšte si kvalifikáciu online z pohodlia domova

Získaná hemofilie - Povědomí o nemoci a její diagnostika
nový kurz

Eozinofilní granulomatóza s polyangiitidou
Autori: doc. MUDr. Martina Doubková, Ph.D.

Všetky kurzy
Prihlásenie
Zabudnuté heslo

Zadajte e-mailovú adresu, s ktorou ste vytvárali účet. Budú Vám na ňu zasielané informácie k nastaveniu nového hesla.

Prihlásenie

Nemáte účet?  Registrujte sa

#ADS_BOTTOM_SCRIPTS#