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• W2088446422 endingPage "370" @default.
• W2088446422 startingPage "337" @default.
• W2088446422 abstract "The Pisco Formation in Peru contains abundant fossil cetaceans in middle Miocene to lower Pliocene sandstone, siltstone, and tuffaceous and diatomaceous mudstone. Fossil whales are especially abundant in the uppermost diatomaceous units. Most specimens are well articulated or partially disarticulated but associated. Degree of preservation is exceptionally high and uniform among articulated and disarticulated specimens and on the lower and upper surfaces of the bones. Some specimens have baleen preserved in anatomical position. Bones show no evidence of bioerosion by macro- or micro-invertebrates, except for a very limited amount of microbial borings. Diatomaceous layers seem to lack bioturbation. However, bioturbation did occur in a few tuffaceous silty and sandy layers of the lower part of the formation. Shark teeth are found associated with many of the specimens; however, despite abundance of whale skeletons, shark tooth marks are extremely rare. Several lines of evidence indicate that sediments and whales were deposited in a shallow-to-deep shelf environment (an embayment), and not in a beach environment. The thick diatomaceous successions record conditions of strong ocean upwelling indicated by the abundant occurrence of the diatom species Thalassionema nitzschioides. The exceptional preservation of diatom frustules suggests that they reached the seafloor very rapidly and were not successively reworked. The hundreds of whale specimens found, their excellent preservation, and their high degree of articulation make the Pisco Formation fossil whales the best representative assemblage of fossil Mysticeti known so far. The abundance of whale skeletons and other vertebrates in the diatomaceous beds, their excellent preservation, including evidence that soft tissue (baleen) was still present at burial, and the degree of articulation, point to frequent mortalities followed by rapid sedimentation that prevented decay of the skeletons and colonization by invertebrates. Sedimentation rates appear much higher than rates inferred from some other modern and ancient settings where whale skeletons have been found." @default.
• W2088446422 created "2016-06-24" @default.
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• W2088446422 date "2015-01-01" @default.
• W2088446422 modified "2023-10-12" @default.
• W2088446422 title "Taphonomy and paleoenvironmental conditions of deposition of fossil whales in the diatomaceous sediments of the Miocene/Pliocene Pisco Formation, southern Peru—A new fossil-lagerstätte" @default.
• W2088446422 cites W1524311637 @default.
• W2088446422 cites W1964570595 @default.
• W2088446422 cites W1964609795 @default.
• W2088446422 cites W1975897702 @default.
• W2088446422 cites W1979570755 @default.
• W2088446422 cites W1984370748 @default.
• W2088446422 cites W1988421519 @default.
• W2088446422 cites W1993761337 @default.
• W2088446422 cites W2000581211 @default.
• W2088446422 cites W2002864668 @default.
• W2088446422 cites W2003350691 @default.
• W2088446422 cites W2004360731 @default.
• W2088446422 cites W2005148919 @default.
• W2088446422 cites W2005477394 @default.
• W2088446422 cites W2007053577 @default.
• W2088446422 cites W2011964019 @default.
• W2088446422 cites W2012680177 @default.
• W2088446422 cites W2016584511 @default.
• W2088446422 cites W2016675261 @default.
• W2088446422 cites W2016988723 @default.
• W2088446422 cites W2024464056 @default.
• W2088446422 cites W2024525605 @default.
• W2088446422 cites W2028631292 @default.
• W2088446422 cites W2029639849 @default.
• W2088446422 cites W2031262356 @default.
• W2088446422 cites W2033397496 @default.
• W2088446422 cites W2041434947 @default.
• W2088446422 cites W2044103124 @default.
• W2088446422 cites W2049261065 @default.
• W2088446422 cites W2056849071 @default.
• W2088446422 cites W2057667623 @default.
• W2088446422 cites W2059588894 @default.
• W2088446422 cites W2060012941 @default.
• W2088446422 cites W2062025378 @default.
• W2088446422 cites W2062868131 @default.
• W2088446422 cites W2066096472 @default.
• W2088446422 cites W2069118672 @default.
• W2088446422 cites W2069667345 @default.
• W2088446422 cites W2075486975 @default.
• W2088446422 cites W2077941204 @default.
• W2088446422 cites W2082136813 @default.
• W2088446422 cites W2082456920 @default.
• W2088446422 cites W2092625189 @default.
• W2088446422 cites W2092640147 @default.
• W2088446422 cites W2096522903 @default.
• W2088446422 cites W2100744802 @default.
• W2088446422 cites W2111346368 @default.
• W2088446422 cites W2111944730 @default.
• W2088446422 cites W2114807610 @default.
• W2088446422 cites W2114814282 @default.
• W2088446422 cites W2115874504 @default.
• W2088446422 cites W2120331284 @default.
• W2088446422 cites W2121039225 @default.
• W2088446422 cites W2122729664 @default.
• W2088446422 cites W2126904020 @default.
• W2088446422 cites W2128509875 @default.
• W2088446422 cites W2128532168 @default.
• W2088446422 cites W2128996139 @default.
• W2088446422 cites W2133985840 @default.
• W2088446422 cites W2147305938 @default.
• W2088446422 cites W2148728587 @default.
• W2088446422 cites W2151239452 @default.
• W2088446422 cites W2151520827 @default.
• W2088446422 cites W2154273520 @default.
• W2088446422 cites W2155894140 @default.
• W2088446422 cites W2259264654 @default.
• W2088446422 cites W2346470945 @default.
• W2088446422 cites W2487864689 @default.
• W2088446422 cites W2493502125 @default.
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• W2088446422 doi "https://doi.org/10.1016/j.palaeo.2014.09.029" @default.
• W2088446422 hasPublicationYear "2015" @default.
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