PMID-sentid	Pub_year	Sent_text		comp_official_name	comp_offsetprotein_name	organism	prot_offset
25639080-0	2014	[Distribution, flux and biological consumption of carbon monoxide in the East China Sea and the South Yellow Sea in summer].	Carbon Monoxide	50-65	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	84-87	
25639080-0	2014	[Distribution, flux and biological consumption of carbon monoxide in the East China Sea and the South Yellow Sea in summer].	Carbon Monoxide	50-65	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	109-112	
16917701-6	2006	The distribution of surface CO concentration (ppb) derived from MOPITT (Measurement of Pollution in the Troposphere) showed high CO levels over the East/Japan Sea on April 10, 2000 when the largest forest fires occurred along the east coast of Korea.	Carbon Monoxide	28-30	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	159-162	
470070-6	1979	The carbon monoxide standards for sea level are probably too lenient for an altitude of 1,500 m and above.	Carbon Monoxide	4-19	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	34-37	
21012584-0	1946	The effect of oxygen pressure on the uptake of carbon monoxide by man at sea level and at altitude.	Carbon Monoxide	47-62	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	73-76	
22619938-0	2011	[Distribution, flux and photoproduction of carbon monoxide in the Yellow Sea and the Bohai Sea in spring].	Carbon Monoxide	43-58	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	73-76	
22619938-8	2011	Using SMARTS2 spectral irradiance model to estimate CO production, the photoproduction rate of CO was 54.60 micromol x (m2 x d)(-1) and the photoproduction of carbon in the Yellow Sea and the Bohai Sea was 26.95 x 10(9) g in spring.	Carbon Monoxide	52-54	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	180-183	
22619938-8	2011	Using SMARTS2 spectral irradiance model to estimate CO production, the photoproduction rate of CO was 54.60 micromol x (m2 x d)(-1) and the photoproduction of carbon in the Yellow Sea and the Bohai Sea was 26.95 x 10(9) g in spring.	Carbon Monoxide	52-54	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	198-201	
21601237-7	2011	On the contrary, the lower O(3) and CO levels found in summer were due to the marine air masses originating from the Philippine Sea and Pacific Ocean.	Carbon Monoxide	36-38	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	128-131