{"title":"“吸血鬼游戏改变者”——光降解改变了对地质样品中多环芳烃起源的解释","authors":"Adam Zakrzewski, Marta Waliczek","doi":"10.1016/j.gloplacha.2025.105035","DOIUrl":null,"url":null,"abstract":"<div><div>Despite minor sources being identified in phytoplankton and as a result of diagenetic processes, polycyclic aromatic hydrocarbons (PAHs) are well-established compounds, which are frequently used as combustion markers. The characteristic distributions of certain PAHs illustrated in several diagnostic plots are used to differentiate between pyrogenic and non-pyrogenic PAHs. These plots do not show the influence of photodegradation, which can hinder the proper interpretation of the origin of PAHs. Differences of up to three weeks in how PAHs resist photodegradation can change their distribution, leading to the coexistence of typically pyrogenic and non-pyrogenic indications. Despite its undoubted role, photodegradation was not discussed as a factor in modelling the distribution of PAHs within geological samples. The results of extensive molecular (GC–MS) and petrological surveys show that the analysed Early-Middle Jurassic (J<sub>1</sub>-J<sub>2</sub>) and Early Cretaceous (Cr<sub>1</sub>) strata contain broad (2- to 7-ring) PAHs distributions, suggesting their pyrogenic origin, which is accompanied by the domination of inertinite group macerals. J<sub>1</sub>-J<sub>2</sub> and Cr<sub>1</sub> strata are differentiated by the role of smoke-derived PAHs. LMW/Total ratio shows that smoke-derived PAHs are more common within the Cr<sub>1</sub> strata. Simultaneously, most Cr<sub>1</sub> strata are characterised by an unobvious distribution of 4-ring PAHs showing the coexistence of typically pyrogenic and non-pyrogenic values of the indicators used. The newly proposed fire temperature index shows that the average paleo-wildfire temperature was 273–425 °C with no differentiation between J<sub>1</sub>-J<sub>2</sub> and Cr<sub>1</sub> strata. This means that photodegradation is an important factor controlling 4-ring PAHs distribution and that unobvious PAHs distribution can be interpreted as a signal from a significant amount of photodegraded, smoke-derived PAHs. Conducted analyses suggest that 5–7 ring PAHs were not photodegraded in a significant way.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"254 ","pages":"Article 105035"},"PeriodicalIF":4.0000,"publicationDate":"2025-08-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"‘Vampirious gamechanger’ — photodegradation changes the interpretation of the origin of polycyclic aromatic hydrocarbons in geological samples\",\"authors\":\"Adam Zakrzewski, Marta Waliczek\",\"doi\":\"10.1016/j.gloplacha.2025.105035\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Despite minor sources being identified in phytoplankton and as a result of diagenetic processes, polycyclic aromatic hydrocarbons (PAHs) are well-established compounds, which are frequently used as combustion markers. The characteristic distributions of certain PAHs illustrated in several diagnostic plots are used to differentiate between pyrogenic and non-pyrogenic PAHs. These plots do not show the influence of photodegradation, which can hinder the proper interpretation of the origin of PAHs. Differences of up to three weeks in how PAHs resist photodegradation can change their distribution, leading to the coexistence of typically pyrogenic and non-pyrogenic indications. Despite its undoubted role, photodegradation was not discussed as a factor in modelling the distribution of PAHs within geological samples. The results of extensive molecular (GC–MS) and petrological surveys show that the analysed Early-Middle Jurassic (J<sub>1</sub>-J<sub>2</sub>) and Early Cretaceous (Cr<sub>1</sub>) strata contain broad (2- to 7-ring) PAHs distributions, suggesting their pyrogenic origin, which is accompanied by the domination of inertinite group macerals. J<sub>1</sub>-J<sub>2</sub> and Cr<sub>1</sub> strata are differentiated by the role of smoke-derived PAHs. LMW/Total ratio shows that smoke-derived PAHs are more common within the Cr<sub>1</sub> strata. Simultaneously, most Cr<sub>1</sub> strata are characterised by an unobvious distribution of 4-ring PAHs showing the coexistence of typically pyrogenic and non-pyrogenic values of the indicators used. The newly proposed fire temperature index shows that the average paleo-wildfire temperature was 273–425 °C with no differentiation between J<sub>1</sub>-J<sub>2</sub> and Cr<sub>1</sub> strata. This means that photodegradation is an important factor controlling 4-ring PAHs distribution and that unobvious PAHs distribution can be interpreted as a signal from a significant amount of photodegraded, smoke-derived PAHs. Conducted analyses suggest that 5–7 ring PAHs were not photodegraded in a significant way.</div></div>\",\"PeriodicalId\":55089,\"journal\":{\"name\":\"Global and Planetary Change\",\"volume\":\"254 \",\"pages\":\"Article 105035\"},\"PeriodicalIF\":4.0000,\"publicationDate\":\"2025-08-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Global and Planetary Change\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0921818125003443\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Global and Planetary Change","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0921818125003443","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
‘Vampirious gamechanger’ — photodegradation changes the interpretation of the origin of polycyclic aromatic hydrocarbons in geological samples
Despite minor sources being identified in phytoplankton and as a result of diagenetic processes, polycyclic aromatic hydrocarbons (PAHs) are well-established compounds, which are frequently used as combustion markers. The characteristic distributions of certain PAHs illustrated in several diagnostic plots are used to differentiate between pyrogenic and non-pyrogenic PAHs. These plots do not show the influence of photodegradation, which can hinder the proper interpretation of the origin of PAHs. Differences of up to three weeks in how PAHs resist photodegradation can change their distribution, leading to the coexistence of typically pyrogenic and non-pyrogenic indications. Despite its undoubted role, photodegradation was not discussed as a factor in modelling the distribution of PAHs within geological samples. The results of extensive molecular (GC–MS) and petrological surveys show that the analysed Early-Middle Jurassic (J1-J2) and Early Cretaceous (Cr1) strata contain broad (2- to 7-ring) PAHs distributions, suggesting their pyrogenic origin, which is accompanied by the domination of inertinite group macerals. J1-J2 and Cr1 strata are differentiated by the role of smoke-derived PAHs. LMW/Total ratio shows that smoke-derived PAHs are more common within the Cr1 strata. Simultaneously, most Cr1 strata are characterised by an unobvious distribution of 4-ring PAHs showing the coexistence of typically pyrogenic and non-pyrogenic values of the indicators used. The newly proposed fire temperature index shows that the average paleo-wildfire temperature was 273–425 °C with no differentiation between J1-J2 and Cr1 strata. This means that photodegradation is an important factor controlling 4-ring PAHs distribution and that unobvious PAHs distribution can be interpreted as a signal from a significant amount of photodegraded, smoke-derived PAHs. Conducted analyses suggest that 5–7 ring PAHs were not photodegraded in a significant way.
期刊介绍:
The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems.
Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged.
Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.