Biblioteca Digital

939 resultados para parasite marker

(Table A4) Distribution of Pleistocene calcareous nannofossil marker species and morphotypes at ODP Hole 177-1091A from Meteor Rise, South Atlantic

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(Table A5) Distribution of Pleistocene calcareous nannofossil marker species and morphotypes at ODP Site 177-1092 from Meteor Rise, South Atlantic

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(Table A6) Distribution of Pleistocene calcareous nannofossil marker species and morphotypes at ODP Site 177-1093 from Shona Ridge, South Atlantic

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(Table A1) Distribution of Pleistocene calcareous nannofossil marker species and morphotypes at ODP Hole 177-1088B from Agulhas Ridge, South Atlantic

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(Table A2) Distribution of Pleistocene calcareous nannofossil marker species and morphotypes at ODP Site 177-1089 from Agulhas Ridge, South Atlantic

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(Table A3) Distribution of Pleistocene calcareous nannofossil marker species and morphotypes at ODP Site 177-1090 from Agulhas Ridge, South Atlantic

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(Table A2) Abundance of nannofossil marker species and morphotypes in sediment core PS2076-3 from the Atlantic sector of the Southern Ocean

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(Table A1) Abundance of nannofossil marker species and morphotypes in sediment core PS2487-6 from the Atlantic sector of the Southern Ocean

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(Table A4) Abundance of nannofossil marker species and morphotypes in sediment core PS2703-1 from the Pacific sector of the Southern Ocean

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(Table A5) Abundance of nannofossil marker species and morphotypes in sediment core PS2708-1 from the Pacific sector of the Southern Ocean

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Age model tie points (bio-events, tephra marker, d18O, 14C) for sites GeoB14403 and GeoB14414

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Trace element analysis of selected glass shards from marine marker tephra Y-7 in core GeoB14403-8

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Major element analysis of selected glass shards from marine marker tephra Y-7 in core GeoB14403-8

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EPOCA Svalbard 2010 mesocosm experiment: depth-integrated (0-12m) phytoplankton community composition using marker pigments (CHEMTAX)

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(Table 1) Occurrence of sapropels and marker layers in ODP Site 160-964 in the eastern Mediterranean Sea

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