PMID-sentid	Pub_year	Sent_text		comp_official_name	comp_offsetprotein_name	organism	prot_offset
14973610-1	2004	We demonstrate here an alternative scheme for C(1) coupling by way of methane bromination, followed by concurrent bromomethane condensation and quantitative HBr neutralization; regeneration of the metal oxide with O(2) with recovery of Br(2) completes the cycle.	Methane	70-77	heterogeneous nuclear ribonucleoprotein C	Homo sapiens	46-50	
15876569-6	2005	This suggests that, although extant methanogens produce methane from various substrates (CO(2), formate, acetate, methylated C-1 compounds), these archaea have a core of conserved enzymes that have undergone little evolutionary change.	Methane	56-63	heterogeneous nuclear ribonucleoprotein C	Homo sapiens	125-128	
101517-2	1978	Suspensions of methane-grown cells of this organism oxidized C-1 compounds (methane, methanol, formaldehyde, formate); hydrocarbons (ethane, propane); primary alcohols (ethanol, propanol); primary aldehydes (acetaldehyde, propionaldehyde); alkenes (ethylene, propylene); dimethylether; and organic acids (acetate, malate, succinate, isocitrate).	Methane	15-22	heterogeneous nuclear ribonucleoprotein C	Homo sapiens	61-64	
35601339-4	2022	Thermodynamically, methane is the most favorable product in a reaction system containing CO, CO2, and H2, as well as C1-4 alkanes, alkenes, and alcohols.	Methane	19-26	heterogeneous nuclear ribonucleoprotein C	Homo sapiens	117-121	
101517-8	1978	Extracts of methane-grown, but not succinate-grown, cells contained the key enzymes of the serine pathway, hydroxypyruvate reductase and malate lyase, indicating that the enzymes of C-1 assimilation are induced only during growth on C-1 compounds.	Methane	12-19	heterogeneous nuclear ribonucleoprotein C	Homo sapiens	182-185	
101517-8	1978	Extracts of methane-grown, but not succinate-grown, cells contained the key enzymes of the serine pathway, hydroxypyruvate reductase and malate lyase, indicating that the enzymes of C-1 assimilation are induced only during growth on C-1 compounds.	Methane	12-19	heterogeneous nuclear ribonucleoprotein C	Homo sapiens	233-236	
27682076-3	2015	C-1 compounds such as methane and methanol are important intermediates in the deep subsurface carbon cycle, and electron acceptors such as sulphate are critical components of oxidation processes.	Methane	22-29	heterogeneous nuclear ribonucleoprotein C	Homo sapiens	0-3	
27682076-6	2015	Our results show that deep subsurface microbes exist in dormant states but rapidly reactivate their transcription and respiration systems in the presence of C-1 substrates, particularly methane.	Methane	186-193	heterogeneous nuclear ribonucleoprotein C	Homo sapiens	157-160