Warming-related increases in soil CO2 efflux are explained by increased below-ground carbon flux (Record no. 50336)
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| fixed length control field | 02021nam a2200217Ia 4500 |
| 003 - CONTROL NUMBER IDENTIFIER | |
| control field | MX-MdCICY |
| 005 - DATE AND TIME OF LATEST TRANSACTION | |
| control field | 20250625160146.0 |
| 040 ## - CATALOGING SOURCE | |
| Transcribing agency | CICY |
| 090 ## - LOCALLY ASSIGNED LC-TYPE CALL NUMBER (OCLC); LOCAL CALL NUMBER (RLIN) | |
| Classification number (OCLC) (R) ; Classification number, CALL (RLIN) (NR) | B-16162 |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION | |
| fixed length control field | 250602s9999 xx |||||s2 |||| ||und|d |
| 245 10 - TITLE STATEMENT | |
| Title | Warming-related increases in soil CO2 efflux are explained by increased below-ground carbon flux |
| 490 0# - SERIES STATEMENT | |
| Volume/sequential designation | Nature Climate Change, 4(9), p.822-827, 2014 |
| 520 3# - SUMMARY, ETC. | |
| Summary, etc. | The universally observed exponential increase in soil-surface CO 2 efflux ('soil respiration'; F S)with increasing temperature has led to speculation that global warming will accelerate soil-organic-carbon (SOC)decomposition, reduce SOC storage, and drive a positive feedback to future warming. However, interpreting temperature-F S relationships, and so modelling terrestrial carbon balance in a warmer world, is complicated by the many sources of respired carbon that contribute to F S (ref.)and a poor understanding of how temperature influences SOC decomposition rates. Here we quantified F S, litterfall, bulk SOC and SOC fraction size and turnover, and total below-ground carbon flux (TBCF)across a highly constrained 5.2 °C mean annual temperature (MAT)gradient in tropical montane wet forest. From these, we determined that: increases in TBCF and litterfall explain >90 percent of the increase in F S with MAT; bulk SOC and SOC fraction size and turnover rate do not vary with MAT; and increases in TBCF and litterfall do not influence SOC storage or turnover on century to millennial timescales. This gradient study shows that for tropical montane wet forest, long-term and whole-ecosystem warming accelerates below-ground carbon processes with no apparent impact on SOC storage. |
| 650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | CARBON FLUX |
| 700 12 - ADDED ENTRY--PERSONAL NAME | |
| Personal name | Giardina, C.P. |
| 700 12 - ADDED ENTRY--PERSONAL NAME | |
| Personal name | Litton, C.M. |
| 700 12 - ADDED ENTRY--PERSONAL NAME | |
| Personal name | Crow, S.E. |
| 700 12 - ADDED ENTRY--PERSONAL NAME | |
| Personal name | Asner, G.P. |
| 856 40 - ELECTRONIC LOCATION AND ACCESS | |
| Uniform Resource Identifier | <a href="https://drive.google.com/file/d/1yqdOT35x5QHtqXZZmkWBtHbYuIEaaudE/view?usp=drivesdk">https://drive.google.com/file/d/1yqdOT35x5QHtqXZZmkWBtHbYuIEaaudE/view?usp=drivesdk</a> |
| Public note | Para ver el documento ingresa a Google con tu cuenta: @cicy.edu.mx |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| Source of classification or shelving scheme | Clasificación local |
| Koha item type | Documentos solicitados |
| Lost status | Source of classification or shelving scheme | Damaged status | Not for loan | Collection | Home library | Current library | Shelving location | Date acquired | Total checkouts | Full call number | Date last seen | Price effective from | Koha item type |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Clasificación local | Ref1 | CICY | CICY | Documento préstamo interbibliotecario | 25.06.2025 | B-16162 | 25.06.2025 | 25.06.2025 | Documentos solicitados |
