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新泽西州埃德尔曼化石公园霍纳stown组海绿石浅海沉积物中脊椎动物化石的软组织和生物分子保存

Soft Tissue and Biomolecular Preservation in Vertebrate Fossils from Glauconitic, Shallow Marine Sediments of the Hornerstown Formation, Edelman Fossil Park, New Jersey.

作者信息

Voegele Kristyn K, Boles Zachary M, Ullmann Paul V, Schroeter Elena R, Zheng Wenxia, Lacovara Kenneth J

机构信息

Department of Geology, Rowan University, Glassboro, NJ 08028, USA.

Jean and Ric Edelman Fossil Park, Rowan University, Mantua Township, NJ 08080, USA.

出版信息

Biology (Basel). 2022 Aug 2;11(8):1161. doi: 10.3390/biology11081161.

DOI:10.3390/biology11081161
PMID:36009787
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9405258/
Abstract

Endogenous biomolecules and soft tissues are known to persist in the fossil record. To date, these discoveries derive from a limited number of preservational environments, (e.g., fluvial channels and floodplains), and fossils from less common depositional environments have been largely unexplored. We conducted paleomolecular analyses of shallow marine vertebrate fossils from the Cretaceous-Paleogene Hornerstown Formation, an 80-90% glauconitic greensand from Jean and Ric Edelman Fossil Park in Mantua Township, NJ. Twelve samples were demineralized and found to yield products morphologically consistent with vertebrate osteocytes, blood vessels, and bone matrix. Specimens from these deposits that are dark in color exhibit excellent histological preservation and yielded a greater recovery of cells and soft tissues, whereas lighter-colored specimens exhibit poor histology and few to no cells/soft tissues. Additionally, a well-preserved femur of the marine crocodilian was found to have retained endogenous collagen I by immunofluorescence and enzyme-linked immunosorbent assays. Our results thus not only corroborate previous findings that soft tissue and biomolecular recovery from fossils preserved in marine environments are possible but also expand the range of depositional environments documented to preserve endogenous biomolecules, thus broadening the suite of geologic strata that may be fruitful to examine in future paleomolecular studies.

摘要

已知内源性生物分子和软组织会保存在化石记录中。迄今为止,这些发现来自有限数量的保存环境(例如,河流渠道和洪泛平原),而来自不太常见沉积环境的化石在很大程度上尚未得到探索。我们对来自白垩纪-古近纪霍纳斯敦组的浅海脊椎动物化石进行了古分子分析,该地层是新泽西州曼图亚镇让和里克·埃德尔曼化石公园80%-90%的海绿石绿砂。对12个样本进行了脱矿处理,发现产生的产物在形态上与脊椎动物的骨细胞、血管和骨基质一致。这些沉积物中颜色较深的标本显示出极佳的组织学保存,细胞和软组织的回收率更高,而颜色较浅的标本组织学较差,几乎没有或没有细胞/软组织。此外,通过免疫荧光和酶联免疫吸附测定法发现,一只保存完好的海鳄股骨保留了内源性I型胶原蛋白。因此,我们的结果不仅证实了先前的发现,即在海洋环境中保存的化石有可能回收软组织和生物分子,而且还扩大了记录到保存内源性生物分子的沉积环境范围,从而拓宽了未来古分子研究中可能有成果进行研究的地质地层类别。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/eaef5b1bfb09/biology-11-01161-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/2414f094949d/biology-11-01161-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/6fb6d6785fc1/biology-11-01161-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/eca16925d875/biology-11-01161-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/10f8732a71b4/biology-11-01161-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/d3c3cd951a56/biology-11-01161-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/0c8dab1197af/biology-11-01161-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/eaef5b1bfb09/biology-11-01161-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/2414f094949d/biology-11-01161-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/6fb6d6785fc1/biology-11-01161-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/eca16925d875/biology-11-01161-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/10f8732a71b4/biology-11-01161-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/d3c3cd951a56/biology-11-01161-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/0c8dab1197af/biology-11-01161-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4031/9405258/eaef5b1bfb09/biology-11-01161-g007.jpg

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