TY  - JOUR

T1  - Late Holocene methane rise caused by orbitally controlled increase in tropical sources.

JO  - Nature

PY  - 2011/02/03

AU  - Singarayer JS

AU  - Valdes PJ

AU  - Friedlingstein P

AU  - Nelson S

AU  - Beerling DJ

ED  - 

DO  - DOI: 10.1038/nature09739

VL  - 470

IS  - 7332

SP  - 82

EP  - 85

Y2  - 2024/12/22

ER  -