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Biofacies Analysis of Zanclean Sediments in Virginia: Unraveling the Past Through Benthic Foraminifera

Early Pliocene sedimentary deposits are exposed at the surface along the James and York Rivers, across southeastern Virginia. The Zanclean age (5.33–3.60 Ma) Sunken Meadow Member of the Yorktown Formation records a relatively large-scale marine transgression in the Salisbury Embayment. A total of 15 samples were collected from an outcrop near Spring Grove, VA, for grain-size analysis and to document benthic and planktic foraminiferal assemblages. The sediments are generally moderately well-sorted, shelly fine sands. A total of 48 benthic taxa were recorded from the Sunken Meadow Member, though only 14 taxa occurred in proportions high enough to be included in the Q-mode cluster analysis (>3% of the total assemblage). Low numbers of planktic foraminifera indicate relatively shallow water deposition. Biofacies analysis shows three distinct biofacies groups in the Sunken Meadow Member and the benthic foraminiferal community shifts throughout the unit are indicative of changes in nutrient availability, surface productivity, and bottom water oxygenation. The results indicate a middle to outer neritic depositional environment similar to modern conditions found south of Cape Hatteras, NC.

Ketersediaan
#
Perpustakaan BIG (Eksternal Harddisk) 550
376
Tersedia
Informasi Detail
Judul Seri
Geosciences
No. Panggil
550
Penerbit
Switzerland : MPDI.,
Deskripsi Fisik
17 hlm PDF, 2.059 KB
Bahasa
Inggris
ISBN/ISSN
2076-3263
Klasifikasi
550
Tipe Isi
text
Tipe Media
-
Tipe Pembawa
online resource
Edisi
Vol.15, Issue 2, February 2025
Subjek
Zanclean
benthic foraminifera
Atlantic Ocean
Info Detail Spesifik
Geosciences
Pernyataan Tanggungjawab
Versi lain/terkait

Tidak tersedia versi lain

Lampiran Berkas
  • Biofacies Analysis of Zanclean Sediments in Virginia: Unraveling the Past Through Benthic Foraminifera
    Early Pliocene sedimentary deposits are exposed at the surface along the James and York Rivers, across southeastern Virginia. The Zanclean age (5.33–3.60 Ma) Sunken Meadow Member of the Yorktown Formation records a relatively large-scale marine transgression in the Salisbury Embayment. A total of 15 samples were collected from an outcrop near Spring Grove, VA, for grain-size analysis and to document benthic and planktic foraminiferal assemblages. The sediments are generally moderately well-sorted, shelly fine sands. A total of 48 benthic taxa were recorded from the Sunken Meadow Member, though only 14 taxa occurred in proportions high enough to be included in the Q-mode cluster analysis (>3% of the total assemblage). Low numbers of planktic foraminifera indicate relatively shallow water deposition. Biofacies analysis shows three distinct biofacies groups in the Sunken Meadow Member and the benthic foraminiferal community shifts throughout the unit are indicative of changes in nutrient availability, surface productivity, and bottom water oxygenation. The results indicate a middle to outer neritic depositional environment similar to modern conditions found south of Cape Hatteras, NC.
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