4.7 Article

Life and reproduction of titanosaurians: Isotopic hallmark of mid-palaeolatitude eggshells and its significance for body temperature, diet, and nesting

期刊

CHEMICAL GEOLOGY
卷 583, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.chemgeo.2021.120452

关键词

Titanosaur eggs; Stable isotopes; Clumped isotopes; Late Cretaceous; NW Argentina

资金

  1. CRILAR
  2. Secretaria de Cultura de La Rioja
  3. Municipalidad de Sanagasta and Tama
  4. Gobierno de La Rioja
  5. Quebrada de Santo Domingo
  6. Jurassic Foundation
  7. Paleontological Society
  8. Agencia Nacional de Promocion Cientifica y Tecnologica [ANPCyT2012-0421, ANPCyT 2018-01211]
  9. Proyecto Sanagasta-Tama 2007-2010 (Gobierno de La Rioja)

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This study investigated the stable isotope compositions of titanosaurian eggshells, identifying a typical isotopic signature for well-preserved eggshells and confirming that titanosaurians were warm-blooded animals mainly feeding on C3 plants, reproducing in drier conditions. The isotopic data are consistent with those from other mid-palaeolatitude nesting sites worldwide.
Eggshells represent an important part of the fossil record of Titanosauria (Dinosauria - Neosaumpoda) and their stable isotope compositions are valuable palaeoenvimnmental proxies. A new set of conventional (delta O-18 and delta C-13) and clumped (Delta(47)) stable isotope compositions of titanosaurian eggshells is presented, together with that of a bone and a single associated tooth, sampled in three Late Cretaceous nesting sites from La Rioja Province, NW Argentina. The preservation state of the fossils was first evaluated using optical and analytical techniques, such as transmitted light and optical cathodoluminescence (CL) microscopy, energy dispersive X-ray spectroscopy (EDX), and laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS). The isotopic compositions of the fossils were then compared to those of associated carbonate rocks and nodules, hydrothermal calcite and quartz, and those reported for eggshells from other nesting sites worldwide. This large, combined sample set allows us to define an isotopic hallmark (delta C-13(VPDB )= -15 to -11 parts per thousand; delta O-18(VSMOV) = 27 to 33 parts per thousand) typical for well-preserved mid-palaeolatitude titanosaurian eggshells. This hallmark is intended to identify the oological specimens best suited for palaeoenvimnmental reconstructions, for instance in museum collection samples that may lack associated abiogenic materials such as host rocks. In addition, our isotopic data support that titanosaurians were animals with an elevated body temperature, mainly feeding on C3 plants, and reproducing under conditions more arid than the long-term average. The data are in excellent agreement with the isotopic data reported from other mid-palaeolatitude nesting sites around the world, indicating that titanosaurians needed similar environmental conditions to reproduce, regardless of the palaeogeographic location of their habitat. Finally, we raise the question whether titanosaurians experienced reproduction-related fasting, as noted for several extant vertebrates, and discuss the complexity of interpreting Delta(47)-derived temperatures, despite very consistent bulk isotopic data.

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