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 - 2025/07/30 ER -