This report documents phytoliths (siliceous plant fossils) in 16 samples from the Cape Roberts Project core (CRP-1), including the first record of two phytolith forms from monocotyledons (Chionochloid (spool) and Elongate) in Antarctica. The phytoliths found are compared with those extracted from extant plants and other Antarctic sedimentary deposits. The phytolith record is also compared with the three floral assemblages indicated by terrestrial palynomorphs for the Miocene and Quaternary sections of the core
Faunas of ammonites and bivalves, aquatic floras of dinocysts and prasinophycean/chlorophycean algae...
The ANDRILL project recovered over 600 m of Plio-Pleistocene sediments within the Ross embayment, An...
Phytoliths are plant-derived mineral bodies. They have been used in a variety of archaeological, env...
Phytoliths (siliceous plant microfossils) have been recovered from Cenozoic sediments (c. 34 to 17 M...
The first core of the Cape Roberts Project, CRP-1, penetrated a Quaternary and lower Miocene section...
Sparse terrestrial palynomorphs (spores and pollen) were recovered from glacigene Lower Miocene and ...
Sites 1165 and 1167 were drilled on the continental slope and rise seaward of Prydz Bay, East Antarc...
Sparse pollen and spores from the lower Miocene section of CRP-1 derive from at least three sources....
Phytoliths are described from deep sea sediments at Site 591 in the southwestern Pacific. Their regi...
The uppermost part of the core in Cape Roberts Project -1 (CRP-1), to 43.55 mbsf, is interpreted to ...
Based on the alternation of diamicts with other clastic sedimentary facies, the predominantly lithif...
Gravity cores taken from five sites in the Nielsen basin, a sinuous trough on the Mac. Robertson she...
ODP Site 1165 recovered around 1000 m of Early to Late Miocene mixed hemi-pelagic sediments from the...
Phytoliths are described from deep sea sediments at Site 591 in the southwestern Pacific. Their regi...
An exceptional triple palynological signal (unusually high abundance of marine, freshwater, and terr...
Faunas of ammonites and bivalves, aquatic floras of dinocysts and prasinophycean/chlorophycean algae...
The ANDRILL project recovered over 600 m of Plio-Pleistocene sediments within the Ross embayment, An...
Phytoliths are plant-derived mineral bodies. They have been used in a variety of archaeological, env...
Phytoliths (siliceous plant microfossils) have been recovered from Cenozoic sediments (c. 34 to 17 M...
The first core of the Cape Roberts Project, CRP-1, penetrated a Quaternary and lower Miocene section...
Sparse terrestrial palynomorphs (spores and pollen) were recovered from glacigene Lower Miocene and ...
Sites 1165 and 1167 were drilled on the continental slope and rise seaward of Prydz Bay, East Antarc...
Sparse pollen and spores from the lower Miocene section of CRP-1 derive from at least three sources....
Phytoliths are described from deep sea sediments at Site 591 in the southwestern Pacific. Their regi...
The uppermost part of the core in Cape Roberts Project -1 (CRP-1), to 43.55 mbsf, is interpreted to ...
Based on the alternation of diamicts with other clastic sedimentary facies, the predominantly lithif...
Gravity cores taken from five sites in the Nielsen basin, a sinuous trough on the Mac. Robertson she...
ODP Site 1165 recovered around 1000 m of Early to Late Miocene mixed hemi-pelagic sediments from the...
Phytoliths are described from deep sea sediments at Site 591 in the southwestern Pacific. Their regi...
An exceptional triple palynological signal (unusually high abundance of marine, freshwater, and terr...
Faunas of ammonites and bivalves, aquatic floras of dinocysts and prasinophycean/chlorophycean algae...
The ANDRILL project recovered over 600 m of Plio-Pleistocene sediments within the Ross embayment, An...
Phytoliths are plant-derived mineral bodies. They have been used in a variety of archaeological, env...