Occurence of marine palynomorphs of sediment core CRP-1 (Table 1) ...
The first core of the Cape Roberts Project, CRP-1, penetrated a Quaternary and lower Miocene section rather than the anticipated Palaeogene sediments. Initial palynologic study was conducted at the Crary Science and Engineering Laboratory, McMurdo Station, concurrent with drilling. Rapid and environ...
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ftdatacite:10.1594/pangaea.54984 2024-09-15T17:47:34+00:00 Occurence of marine palynomorphs of sediment core CRP-1 (Table 1) ... Wrenn, John Hannah, Mike J Raine, J Ian 1998 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.54984 https://doi.pangaea.de/10.1594/PANGAEA.54984 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Depth, top/min Depth, bottom/max Leiosphaeridia sp. Lycopodium spike Tasmanites Cymatiosphaera sp. Vozzhennikovia apertura Impagidinium sp. Indeterminata/varia Sigmopollis sp. Batiacasphaera cooperi Paralecaniella indentata Psilate sphere Foraminifera, linings Spinidinium macmurdoense Operculodinium sp. Micrhystridium sp. Arthropod and annelid parts Spiniferites sp. Lejeunecysta cowiei Brigantedinium pynei Lejeunecysta fallax Alterbidinium cf. asymmetrica Deflandrea antarctica Pterospermella sp. Operculodinium bergmannii Vozzhennikovia cf. apertura Phelodinium cranwelliae Dinoflagellates, total Acritarcha Core wireline system Counting, palynology CRP-1 Sampling/drilling ice Cape Roberts Project CRP dataset Supplementary Dataset Dataset 1998 ftdatacite https://doi.org/10.1594/pangaea.54984 2024-08-01T11:12:47Z The first core of the Cape Roberts Project, CRP-1, penetrated a Quaternary and lower Miocene section rather than the anticipated Palaeogene sediments. Initial palynologic study was conducted at the Crary Science and Engineering Laboratory, McMurdo Station, concurrent with drilling. Rapid and environmentally safe sample processing was made possible by the use of a focused microwave digestion unit that scrubbed acid fumes. In situ and/or reworked dinocysts (dinoflagellate cysts), acritarchs (leiospheres and acanthomorphs), and prasinophyte phycomata are present in the 35 samples studied. Overall, the CRP-1 assemblages are similar to Arctic marine palynomorph assemblages that are used there as ice margin indicators. Some of the acanthomorph acritarchs recovered from the CRP-1 core closely resemble cysts of extant Antarctic autotrophic sea-ice dinoflagellates. It is possible that some of these acanthomorphs are actually dinocysts, and could be used as indicators of sea-ice conditions similar to today.Most of the ... : Supplement to: Wrenn, John; Hannah, Mike J; Raine, J Ian (1998): Diversity and palaeoenvironmental significance of late Cenozoic marine palynomorphs from the CRP-1 Core, Ross Sea, Antarctica. Terra Antartica, 5(3), 553-570 ... Dataset Antarc* Antarctic Antarctica antartic* Foraminifera* Ross Sea Sea ice DataCite |
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language |
English |
topic |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Leiosphaeridia sp. Lycopodium spike Tasmanites Cymatiosphaera sp. Vozzhennikovia apertura Impagidinium sp. Indeterminata/varia Sigmopollis sp. Batiacasphaera cooperi Paralecaniella indentata Psilate sphere Foraminifera, linings Spinidinium macmurdoense Operculodinium sp. Micrhystridium sp. Arthropod and annelid parts Spiniferites sp. Lejeunecysta cowiei Brigantedinium pynei Lejeunecysta fallax Alterbidinium cf. asymmetrica Deflandrea antarctica Pterospermella sp. Operculodinium bergmannii Vozzhennikovia cf. apertura Phelodinium cranwelliae Dinoflagellates, total Acritarcha Core wireline system Counting, palynology CRP-1 Sampling/drilling ice Cape Roberts Project CRP |
spellingShingle |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Leiosphaeridia sp. Lycopodium spike Tasmanites Cymatiosphaera sp. Vozzhennikovia apertura Impagidinium sp. Indeterminata/varia Sigmopollis sp. Batiacasphaera cooperi Paralecaniella indentata Psilate sphere Foraminifera, linings Spinidinium macmurdoense Operculodinium sp. Micrhystridium sp. Arthropod and annelid parts Spiniferites sp. Lejeunecysta cowiei Brigantedinium pynei Lejeunecysta fallax Alterbidinium cf. asymmetrica Deflandrea antarctica Pterospermella sp. Operculodinium bergmannii Vozzhennikovia cf. apertura Phelodinium cranwelliae Dinoflagellates, total Acritarcha Core wireline system Counting, palynology CRP-1 Sampling/drilling ice Cape Roberts Project CRP Wrenn, John Hannah, Mike J Raine, J Ian Occurence of marine palynomorphs of sediment core CRP-1 (Table 1) ... |
topic_facet |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Leiosphaeridia sp. Lycopodium spike Tasmanites Cymatiosphaera sp. Vozzhennikovia apertura Impagidinium sp. Indeterminata/varia Sigmopollis sp. Batiacasphaera cooperi Paralecaniella indentata Psilate sphere Foraminifera, linings Spinidinium macmurdoense Operculodinium sp. Micrhystridium sp. Arthropod and annelid parts Spiniferites sp. Lejeunecysta cowiei Brigantedinium pynei Lejeunecysta fallax Alterbidinium cf. asymmetrica Deflandrea antarctica Pterospermella sp. Operculodinium bergmannii Vozzhennikovia cf. apertura Phelodinium cranwelliae Dinoflagellates, total Acritarcha Core wireline system Counting, palynology CRP-1 Sampling/drilling ice Cape Roberts Project CRP |
description |
The first core of the Cape Roberts Project, CRP-1, penetrated a Quaternary and lower Miocene section rather than the anticipated Palaeogene sediments. Initial palynologic study was conducted at the Crary Science and Engineering Laboratory, McMurdo Station, concurrent with drilling. Rapid and environmentally safe sample processing was made possible by the use of a focused microwave digestion unit that scrubbed acid fumes. In situ and/or reworked dinocysts (dinoflagellate cysts), acritarchs (leiospheres and acanthomorphs), and prasinophyte phycomata are present in the 35 samples studied. Overall, the CRP-1 assemblages are similar to Arctic marine palynomorph assemblages that are used there as ice margin indicators. Some of the acanthomorph acritarchs recovered from the CRP-1 core closely resemble cysts of extant Antarctic autotrophic sea-ice dinoflagellates. It is possible that some of these acanthomorphs are actually dinocysts, and could be used as indicators of sea-ice conditions similar to today.Most of the ... : Supplement to: Wrenn, John; Hannah, Mike J; Raine, J Ian (1998): Diversity and palaeoenvironmental significance of late Cenozoic marine palynomorphs from the CRP-1 Core, Ross Sea, Antarctica. Terra Antartica, 5(3), 553-570 ... |
format |
Dataset |
author |
Wrenn, John Hannah, Mike J Raine, J Ian |
author_facet |
Wrenn, John Hannah, Mike J Raine, J Ian |
author_sort |
Wrenn, John |
title |
Occurence of marine palynomorphs of sediment core CRP-1 (Table 1) ... |
title_short |
Occurence of marine palynomorphs of sediment core CRP-1 (Table 1) ... |
title_full |
Occurence of marine palynomorphs of sediment core CRP-1 (Table 1) ... |
title_fullStr |
Occurence of marine palynomorphs of sediment core CRP-1 (Table 1) ... |
title_full_unstemmed |
Occurence of marine palynomorphs of sediment core CRP-1 (Table 1) ... |
title_sort |
occurence of marine palynomorphs of sediment core crp-1 (table 1) ... |
publisher |
PANGAEA |
publishDate |
1998 |
url |
https://dx.doi.org/10.1594/pangaea.54984 https://doi.pangaea.de/10.1594/PANGAEA.54984 |
genre |
Antarc* Antarctic Antarctica antartic* Foraminifera* Ross Sea Sea ice |
genre_facet |
Antarc* Antarctic Antarctica antartic* Foraminifera* Ross Sea Sea ice |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.54984 |
_version_ |
1810496981455339520 |