First report of amber with spider webs and microbial inclusions from the earliest Cretaceous (c. 140 Ma) of Hastings, Sussex

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First report of amber with spider webs and microbial inclusions from the earliest Cretaceous (c. 140 Ma) of Hastings, Sussex. / Brasier, Martin; Cotton, Laura; Yenney, Ian.

In: Journal of the Geological Society, Vol. 166, No. 6, 2009, p. 989-997.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Brasier, M, Cotton, L & Yenney, I 2009, 'First report of amber with spider webs and microbial inclusions from the earliest Cretaceous (c. 140 Ma) of Hastings, Sussex', Journal of the Geological Society, vol. 166, no. 6, pp. 989-997. https://doi.org/10.1144/0016-76492008-158

APA

Brasier, M., Cotton, L., & Yenney, I. (2009). First report of amber with spider webs and microbial inclusions from the earliest Cretaceous (c. 140 Ma) of Hastings, Sussex. Journal of the Geological Society, 166(6), 989-997. https://doi.org/10.1144/0016-76492008-158

Vancouver

Brasier M, Cotton L, Yenney I. First report of amber with spider webs and microbial inclusions from the earliest Cretaceous (c. 140 Ma) of Hastings, Sussex. Journal of the Geological Society. 2009;166(6):989-997. https://doi.org/10.1144/0016-76492008-158

Author

Brasier, Martin ; Cotton, Laura ; Yenney, Ian. / First report of amber with spider webs and microbial inclusions from the earliest Cretaceous (c. 140 Ma) of Hastings, Sussex. In: Journal of the Geological Society. 2009 ; Vol. 166, No. 6. pp. 989-997.

Bibtex

@article{d8e196b292f94886a011a376f1969ac1,
title = "First report of amber with spider webs and microbial inclusions from the earliest Cretaceous (c. 140 Ma) of Hastings, Sussex",
abstract = "Early Cretaceous amber resins with macroscopic inclusions are extremely rare, as are ambers with inclusions from the parent plant. Here, we report earliest Cretaceous amber resins found within alluvial soils of the Ashdown Formation near Hastings in Sussex. In contrast to younger Cretaceous examples, this Hastings amber was arguably deposited shortly before the emergence of the earliest flowering plant communities c. 140 Ma BP. Preliminary studies reveal plentiful organic inclusions, including vascular tissues, tracheid cells and putative resin ducts of the parent coniferous trees. We also report remarkably preserved soil microbes, including structures comparable with actinobacterial colonies, putative fungal or cyanobacterial filaments, and the earliest examples of spider silk webs. The last includes threads that are twisted, paired and coated with sticky fluid droplets, comparable with those of araneoid spider webs studied by us in modern cherry tree resins. Together, these Hastings amber inclusions became entombed within resins that seeped through the charred bark of coniferous trees subjected to severe fire damage, whose logs were then swept onto fluvial wetlands by floods. Embalming resins of this kind may have evolved to combat damage associated with insects, fungi and widespread forest fires.",
author = "Martin Brasier and Laura Cotton and Ian Yenney",
year = "2009",
doi = "10.1144/0016-76492008-158",
language = "English",
volume = "166",
pages = "989--997",
journal = "Journal of the Geological Society",
issn = "0016-7649",
publisher = "Geological Society Publishing House",
number = "6",

}

RIS

TY - JOUR

T1 - First report of amber with spider webs and microbial inclusions from the earliest Cretaceous (c. 140 Ma) of Hastings, Sussex

AU - Brasier, Martin

AU - Cotton, Laura

AU - Yenney, Ian

PY - 2009

Y1 - 2009

N2 - Early Cretaceous amber resins with macroscopic inclusions are extremely rare, as are ambers with inclusions from the parent plant. Here, we report earliest Cretaceous amber resins found within alluvial soils of the Ashdown Formation near Hastings in Sussex. In contrast to younger Cretaceous examples, this Hastings amber was arguably deposited shortly before the emergence of the earliest flowering plant communities c. 140 Ma BP. Preliminary studies reveal plentiful organic inclusions, including vascular tissues, tracheid cells and putative resin ducts of the parent coniferous trees. We also report remarkably preserved soil microbes, including structures comparable with actinobacterial colonies, putative fungal or cyanobacterial filaments, and the earliest examples of spider silk webs. The last includes threads that are twisted, paired and coated with sticky fluid droplets, comparable with those of araneoid spider webs studied by us in modern cherry tree resins. Together, these Hastings amber inclusions became entombed within resins that seeped through the charred bark of coniferous trees subjected to severe fire damage, whose logs were then swept onto fluvial wetlands by floods. Embalming resins of this kind may have evolved to combat damage associated with insects, fungi and widespread forest fires.

AB - Early Cretaceous amber resins with macroscopic inclusions are extremely rare, as are ambers with inclusions from the parent plant. Here, we report earliest Cretaceous amber resins found within alluvial soils of the Ashdown Formation near Hastings in Sussex. In contrast to younger Cretaceous examples, this Hastings amber was arguably deposited shortly before the emergence of the earliest flowering plant communities c. 140 Ma BP. Preliminary studies reveal plentiful organic inclusions, including vascular tissues, tracheid cells and putative resin ducts of the parent coniferous trees. We also report remarkably preserved soil microbes, including structures comparable with actinobacterial colonies, putative fungal or cyanobacterial filaments, and the earliest examples of spider silk webs. The last includes threads that are twisted, paired and coated with sticky fluid droplets, comparable with those of araneoid spider webs studied by us in modern cherry tree resins. Together, these Hastings amber inclusions became entombed within resins that seeped through the charred bark of coniferous trees subjected to severe fire damage, whose logs were then swept onto fluvial wetlands by floods. Embalming resins of this kind may have evolved to combat damage associated with insects, fungi and widespread forest fires.

U2 - 10.1144/0016-76492008-158

DO - 10.1144/0016-76492008-158

M3 - Journal article

AN - SCOPUS:70350584486

VL - 166

SP - 989

EP - 997

JO - Journal of the Geological Society

JF - Journal of the Geological Society

SN - 0016-7649

IS - 6

ER -

ID: 315595163