PMID-sentid	Pub_year	Sent_text		comp_official_name	comp_offsetprotein_name	organism	prot_offset
20048825-3	1966	For example, a cell length of 1500 cm of CO(2) at 760-mm pressure, equivalent to the CO(2) content in 50,000 m of atmosphere at sea level, transmitted 20% of the energy in the band region from 4.0 micro to 5.5 micro.	co(2)	41-46	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	128-131	
16764526-4	2006	With regard to CO(2) sensitivity, CMS subjects seem to have reset their central CO(2) chemoreceptors to operate around the sea-level resting P(ET(CO2)).	co(2)	15-20	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	123-126	
16764526-4	2006	With regard to CO(2) sensitivity, CMS subjects seem to have reset their central CO(2) chemoreceptors to operate around the sea-level resting P(ET(CO2)).	co(2)	80-85	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	123-126	
20048825-3	1966	For example, a cell length of 1500 cm of CO(2) at 760-mm pressure, equivalent to the CO(2) content in 50,000 m of atmosphere at sea level, transmitted 20% of the energy in the band region from 4.0 micro to 5.5 micro.	co(2)	85-90	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	128-131	
23292932-4	2013	The relationship between CO(2) and sea level we describe portrays the "likely" (68% probability) long-term sea-level response after Earth system adjustment over many centuries.	co(2)	25-30	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	107-110	
23292932-2	2013	Here we use observations from five well-studied time slices covering the last 40 My to identify a well-defined and clearly sigmoidal relationship between atmospheric CO(2) and sea level on geological (near-equilibrium) timescales.	co(2)	166-171	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	176-179	
23292932-4	2013	The relationship between CO(2) and sea level we describe portrays the "likely" (68% probability) long-term sea-level response after Earth system adjustment over many centuries.	co(2)	25-30	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	35-38	
23292932-6	2013	For instance, with CO(2) stabilized at 400-450 ppm (as required for the frequently quoted "acceptable warming" of 2  C), or even at AD 2011 levels of 392 ppm, we infer a likely (68% confidence) long-term sea-level rise of more than 9 m above the present.	co(2)	19-24	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	204-207	
23292932-7	2013	Therefore, our results imply that to avoid significantly elevated sea level in the long term, atmospheric CO(2) should be reduced to levels similar to those of preindustrial times.	co(2)	106-111	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	66-69	
21282152-4	2011	As anthropogenic CO(2) permeates into the ocean, it is making sea water more acidic, to the detriment of surface corals and probably many other calcifiers.	co(2)	17-22	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	62-65	
21282152-7	2011	A curious feedback in the ocean, carbonate compensation, makes it more likely that global warming and sea-level rise will continue for many millennia after CO(2) emissions cease.	co(2)	156-161	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	102-105	
20649907-5	2010	The results showed that a single epsilonproteobacterium, affiliated with the genus Sulfurimonas, and two different members of the gammaproteobacterial sulfur oxidizer (GSO) cluster were responsible for dark CO(2) fixation activities in the upper sulfidic layer of the Black Sea redoxcline.	co(2)	207-212	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	274-277	
18579160-0	2008	Regional scale impacts of distinct CO(2) additions in the North Sea.	co(2)	35-40	S13 erythroblastosis (avian) oncogene homolog	Homo sapiens	64-67