PMID-sentid	Pub_year	Sent_text		comp_official_name	comp_offsetprotein_name	organism	prot_offset
20080721-1	2010	Quantifying atmospheric CO(2) concentrations ([CO(2)](atm)) during Earth"s ancient greenhouse episodes is essential for accurately predicting the response of future climate to elevated CO(2) levels.	co(2)	24-29	ATM serine/threonine kinase	Homo sapiens	12-15	
20080721-1	2010	Quantifying atmospheric CO(2) concentrations ([CO(2)](atm)) during Earth"s ancient greenhouse episodes is essential for accurately predicting the response of future climate to elevated CO(2) levels.	co(2)	47-52	ATM serine/threonine kinase	Homo sapiens	12-15	
20080721-1	2010	Quantifying atmospheric CO(2) concentrations ([CO(2)](atm)) during Earth"s ancient greenhouse episodes is essential for accurately predicting the response of future climate to elevated CO(2) levels.	co(2)	47-52	ATM serine/threonine kinase	Homo sapiens	12-15	
20080721-2	2010	Empirical estimates of [CO(2)](atm) during Paleozoic and Mesozoic greenhouse climates are based primarily on the carbon isotope composition of calcium carbonate in fossil soils.	co(2)	24-29	ATM serine/threonine kinase	Homo sapiens	31-34	
20080721-3	2010	We report that greenhouse [CO(2)](atm) have been significantly overestimated because previously assumed soil CO(2) concentrations during carbonate formation are too high.	co(2)	27-32	ATM serine/threonine kinase	Homo sapiens	34-37	
20080721-3	2010	We report that greenhouse [CO(2)](atm) have been significantly overestimated because previously assumed soil CO(2) concentrations during carbonate formation are too high.	co(2)	109-114	ATM serine/threonine kinase	Homo sapiens	34-37	
20080721-4	2010	More accurate [CO(2)](atm), resulting from better constraints on soil CO(2), indicate that large (1,000s of ppmV) fluctuations in [CO(2)](atm) did not characterize ancient climates and that past greenhouse climates were accompanied by concentrations similar to those projected for A.D. 2100.	co(2)	15-20	ATM serine/threonine kinase	Homo sapiens	22-25	
20080721-4	2010	More accurate [CO(2)](atm), resulting from better constraints on soil CO(2), indicate that large (1,000s of ppmV) fluctuations in [CO(2)](atm) did not characterize ancient climates and that past greenhouse climates were accompanied by concentrations similar to those projected for A.D. 2100.	co(2)	70-75	ATM serine/threonine kinase	Homo sapiens	22-25	
20080721-4	2010	More accurate [CO(2)](atm), resulting from better constraints on soil CO(2), indicate that large (1,000s of ppmV) fluctuations in [CO(2)](atm) did not characterize ancient climates and that past greenhouse climates were accompanied by concentrations similar to those projected for A.D. 2100.	co(2)	70-75	ATM serine/threonine kinase	Homo sapiens	22-25	
18366225-5	2008	The air bubbles are stable for more than 4 days, whereas the CO(2) bubbles are only stable for 1-2 h. We determine the average gas pressure inside the CO(2) bubbles from the IR spectrum in two ways: from the width of the rotational fine structure (P(gas) < 2 atm) and from the intensity in the IR spectrum (P(gas) = 1.1 +/- 0.4 atm).	co(2)	151-156	ATM serine/threonine kinase	Homo sapiens	262-265	
18366225-5	2008	The air bubbles are stable for more than 4 days, whereas the CO(2) bubbles are only stable for 1-2 h. We determine the average gas pressure inside the CO(2) bubbles from the IR spectrum in two ways: from the width of the rotational fine structure (P(gas) < 2 atm) and from the intensity in the IR spectrum (P(gas) = 1.1 +/- 0.4 atm).	co(2)	151-156	ATM serine/threonine kinase	Homo sapiens	331-334