| 000 | 03223nam a22004577a 4500 | ||
|---|---|---|---|
| 999 |
_c136395 _d136395 |
||
| 003 | CR-TuBCO | ||
| 005 | 20220423181832.0 | ||
| 007 | ta | ||
| 008 | 141015t1992 xxu||||| |||| 00| 0 eng d | ||
| 022 | _a1573-2932 | ||
| 022 | _a0049-6979 | ||
| 040 |
_aCR-TuBCO _bspa _cCR-TuBCO |
||
| 041 | _aeng | ||
| 100 |
_9125921 _aTwilley, R.R. _uUniversity of Southwestern Louisiana, Lafayette, USA |
||
| 245 | _aCarbon sinks in mangroves and their implications to carbon budget of tropical coastal ecosystems | ||
| 260 |
_aPaíses Bajos _bKluwer Academic Publishers _c1992 |
||
| 300 |
_a24 páginas _b: 10 ilustraciones, 6 tablas |
||
| 504 | _aBibliografía páginas 283-288 | ||
| 520 | _aNearly 50% of terrigenous materials delivered to the world's oceans are delivered through just twenty-one major river systems. The tropical regions of the biosphere are the most biogeochemically active coastal regions and represent potentially important sinks of C in the biosphere. Rates of net primary productivity and biomass accumulation depend on a combination of global factors such as latitude and local factors such as hydrology. Global estimates of export from coastal wetlands is about 0.08 Pg C/yr compared to input of 0.36 Pg C/yr from rivers to coastal ecosystems. Total allochthonous input of 0.44 Pg C/yr is lower than in situ production of 6.65 Pg C/yr. The trophic condition of coastal ecosystems depends on the fate of this total supply of 7.09 Pg C/yr as either contributing to system respiration, or becoming permanently stored in sediments. Accumulation of carbon in coastal sediments is only 0.41 Pg C/yr; about 6% of the total input. The NEP of coastal wetlands also contribute to the C sink of coastal margins, but the source of this C is part of the terrestrial C exchange with the atmosphere. Accumulation of C in wood and sediments of coastal wetlands is 0.205 Pg C/yr, half the estimate for sequestering of C in coastal sediments. Burial of C in shelf sediments is probably underestimated, particularly in tropical river-dominated coastal margins. Better estimates of these two C sinks in the tropics, coastal wetlands and shelf sediments, is needed to better understand the contribution of coastal ecosystems to the global carbon budget. | ||
| 650 |
_9137963 _aBIOMASA |
||
| 650 |
_9139477 _a CARBONO |
||
| 650 |
_9135397 _aALMACENAMIENTO |
||
| 650 |
_9148477 _aFOTOSINTESIS |
||
| 650 |
_9153819 _aMANGLES |
||
| 650 |
_9136560 _aAREA COSTERA |
||
| 650 |
_95 _aECOSISTEMA |
||
| 650 |
_9143269 _aCURSOS DE AGUA |
||
| 650 |
_9154288 _aMEDICION |
||
| 650 |
_9155109 _a MODELOS |
||
| 650 |
_9160264 _aPRODUCCION DE MADERA |
||
| 650 |
_9145225 _aECUACIONES ALOMETRICAS |
||
| 650 |
_9137965 _aBIOMASA AEREA |
||
| 650 |
_9147939 _aFIJACION DE CARBONO |
||
| 651 | 0 |
_928689 _aPUERTO RICO |
|
| 700 |
_957015 _aChen, R.H. _c (autor/a) _uUniversity of Southwestern Louisiana, Lafayette, USA |
||
| 700 |
_976116 _aHargis, T. _c (autor/a) _uUniversity of Southwestern Louisiana, Lafayette, USA |
||
| 830 |
_aWater, Air, and Soil Pollution _nNúmero 64 (1992) _pAgosto _ppáginas 265-288 |
||
| 856 |
_qpdf _uhttps://link.springer.com/article/10.1007/BF00477106 _yeng |
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| 942 |
_cANA _2ddc |
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