TY - JOUR
T1 - Computational chemical investigation into isorenieratene cyclisation
AU - Van Duin, Adri C.T.
AU - Sinninghe Damsté, Jaap S.
N1 - Funding Information:
This work was supported by a Royal Society Research Fellowship for ACTvD. We thank Prof. William A. Goddard III and members of his group from the Materials and Process Simulation Center, California Institute of Technology, for computational support. We also thank Dr. Kliti Grice and Dr. François Lorant for their constructive review of this manuscript.
PY - 2003
Y1 - 2003
N2 - In sediments, the diaromatic carotenoid isorenieratene can undergo a wide range of molecular transformations, including cyclisation reactions via a Diels-Alder mechanism resulting in either mono- and diaromatic compounds or tetracyclic isorenieratene derivatives. To study these complex diagenetic pathways, we have used molecular dynamics simulations, in concert with a newly developed reactive hydrocarbon force field (ReaxFF). This allows us to simulate the entire cyclisation pathway, including both stable intermediates as well as energy barriers related to transition states. Our simulations indicate that the formation of tetracyclic isorenieratene derivatives is likely to occur via an A-ring initiated reaction mechanism, as the reaction product resulting from A-ring closure is more stable than that derived from B-ring closure. Furthermore, the A-ring initiated tetracyclisation pathways contain one fewer high-energy hydrogen shift step than their B-ring initiated counterparts, indicating that B-ring initiated cyclisation is more likely to result in the formation of monoaromatic compounds. These observations are in excellent agreement with observed distributions of isorenieratene derivatives in sediments and provide a better understanding of the complex diagenetic pathways of isorenieratene.
AB - In sediments, the diaromatic carotenoid isorenieratene can undergo a wide range of molecular transformations, including cyclisation reactions via a Diels-Alder mechanism resulting in either mono- and diaromatic compounds or tetracyclic isorenieratene derivatives. To study these complex diagenetic pathways, we have used molecular dynamics simulations, in concert with a newly developed reactive hydrocarbon force field (ReaxFF). This allows us to simulate the entire cyclisation pathway, including both stable intermediates as well as energy barriers related to transition states. Our simulations indicate that the formation of tetracyclic isorenieratene derivatives is likely to occur via an A-ring initiated reaction mechanism, as the reaction product resulting from A-ring closure is more stable than that derived from B-ring closure. Furthermore, the A-ring initiated tetracyclisation pathways contain one fewer high-energy hydrogen shift step than their B-ring initiated counterparts, indicating that B-ring initiated cyclisation is more likely to result in the formation of monoaromatic compounds. These observations are in excellent agreement with observed distributions of isorenieratene derivatives in sediments and provide a better understanding of the complex diagenetic pathways of isorenieratene.
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U2 - 10.1016/S0146-6380(02)00247-4
DO - 10.1016/S0146-6380(02)00247-4
M3 - Article
AN - SCOPUS:0037242129
SN - 0146-6380
VL - 34
SP - 515
EP - 526
JO - Organic Geochemistry
JF - Organic Geochemistry
IS - 4
ER -