. Bulletins of American paleontology. of ostracodes. Riviere Agoiadiome ^ __^_ irrence of abundant ^ynphisiegiva and Gypaina and local abundance of planktic foramini- fera. "N" zones (Blow, 19(19) are based on planktic foraminifera. In the Las Cahobas Formation, where planktic foraminifera are scarce or absent, only two levels have been marked by the possible lower or upper planktic zones. On the right hand side of the chart a curve indicates suggested relative depth of deposition, based on the distribution of foraminifera and ostracodes. The boundary between "shallow" and
. Bulletins of American paleontology. of ostracodes. Riviere Agoiadiome ^ __^_ irrence of abundant ^ynphisiegiva and Gypaina and local abundance of planktic foramini- fera. "N" zones (Blow, 19(19) are based on planktic foraminifera. In the Las Cahobas Formation, where planktic foraminifera are scarce or absent, only two levels have been marked by the possible lower or upper planktic zones. On the right hand side of the chart a curve indicates suggested relative depth of deposition, based on the distribution of foraminifera and ostracodes. The boundary between "shallow" and "deep" here is about 200 m. Depth Ijpundaries are not the same in all tables, and indicate relative rather than absolute bathymetry. in liiiHi j||i41 j I 111 ,ilJifj I 1 . - , J s I I i I i 111 I Text-figure 5. â Locality map of the area between Hinche and the Riviere Agoiadiome. Samples collected by H, M. Kirk and A. F. Richard- son (KR in Text-fig. 4) without prefix; where available dip i Text-figure 4. â Stratigraphie column of the Rivifere Agoiadiome tion (see Text-fig. 1. sect. A). Ostra code-be a ring samples taken by M. Kirk (K) and H. M. Kirk and A. F. Richardson (KR). .,. 1 â â 1 1 1 " 1 1 > .» 1 > ns 1 1 1 r 1 > j; 1 1 1 1 « 1. 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 'Mil \ 1 1 ">i» â 1 - 1 1 1 1 J ^ y X X -=,. ^\ ^f ThomasBique V ' \r^ o>\k885 KV ' ^---T 13^ h-- ^ \, >K885 Q ^K884 /a ^ '^K883 { J ;.-- \«>-f if A \ ^9 ,w '. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ]
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