Multi-protease analysis of Pleistocene bone proteomes.

Ancient protein analysis is providing new insights into the evolutionary relationships between hominin fossils across the Pleistocene. Protein identification commonly relies on the proteolysis of a protein extract using a single protease, trypsin. As with modern proteome studies, alternative or additional proteases have the potential to increase both proteome size and protein sequence recovery. This could enhance the recovery of phylogenetic information from ancient proteomes. Here we identify 18 novel hominin bone specimens from the Kleine Feldhofer Grotte using MALDI-TOF MS peptide mass fingerprinting of collagen type I. Next, we use one of these hominin bone specimens and three Late Pleistocene Equidae specimens identified in a similar manner and present a comparison of the bone proteome size and protein sequence recovery obtained after using nanoLC-MS/MS and parallel proteolysis using six different proteases, including trypsin. We observe that the majority of the preserved bone proteome is inaccessible to trypsin. We also observe that for proteins recovered consistently across several proteases, protein sequence coverage can be increased significantly by combining peptide identifications from two or more proteases. Our results thereby demonstrate that the proteolysis of Pleistocene proteomes by several proteases has clear advantages when addressing evolutionary questions in palaeoproteomics. SIGNIFICANCE: Maximizing proteome and protein sequence recovery of ancient skeletal proteomes is important when analyzing unique hominin fossils. As with modern proteome studies, palaeoproteomic analysis of Pleistocene bone and dentine samples has almost exclusively used trypsin as its only protease, despite the demonstrated advantages of alternative proteases to increase proteome recovery in modern proteome studies. We demonstrate that Pleistocene bone proteomes can be significantly expanded by using additional proteases beside trypsin, and that this also improves sequence coverage of individual proteins. The use of several alternative proteases beside trypsin therefore has major benefits to maximize the phylogenetic information retrieved from ancient skeletal proteomes.

A draft sequence of the Neandertal genome.

Neandertals, the closest evolutionary relatives of present-day humans, lived in large parts of Europe and western Asia before disappearing 30,000 years ago. We present a draft sequence of the Neandertal genome composed of more than 4 billion nucleotides from three individuals. Comparisons of the Neandertal genome to the genomes of five present-day humans from different parts of the world identify a number of genomic regions that may have been affected by positive selection in ancestral modern humans, including genes involved in metabolism and in cognitive and skeletal development. We show that Neandertals shared more genetic variants with present-day humans in Eurasia than with present-day humans in sub-Saharan Africa, suggesting that gene flow from Neandertals into the ancestors of non-Africans occurred before the divergence of Eurasian groups from each other.

New insights into mid-late Pleistocene fossil hominin paranasal sinus morphology.

Mid-late Pleistocene fossil hominins such as Homo neanderthalensis and H. heidelbergensis are often described as having extensively pneumatized crania compared with modern humans. However, the significance of pneumatization in recognizing patterns of phyletic diversification and/or functional specialization has remained controversial. Here, we test the null hypothesis that the paranasal sinuses of fossil and extant humans and great apes can be understood as biological spandrels, i.e., their morphology reflects evolutionary, developmental, and functional constraints imposed onto the surrounding bones. Morphological description of well-preserved mid-late Pleistocene hominin specimens are contrasted with our comparative sample of modern humans and great apes. Results from a geometric morphometric analysis of the correlation between paranasal sinus and cranial dimensions show that the spandrel hypothesis cannot be refuted. However, visualizing specific features of the paranasal sinus system with methods of biomedical imaging and computer graphics reveals new aspects of patterns of growth and development of fossil hominins.

The Neandertal type site revisited: interdisciplinary investigations of skeletal remains from the Neander Valley, Germany.

The 1856 discovery of the Neandertal type specimen (Neandertal 1) in western Germany marked the beginning of human paleontology and initiated the longest-standing debate in the discipline: the role of Neandertals in human evolutionary history. We report excavations of cave sediments that were removed from the Feldhofer caves in 1856. These deposits have yielded over 60 human skeletal fragments, along with a large series of Paleolithic artifacts and faunal material. Our analysis of this material represents the first interdisciplinary analysis of Neandertal remains incorporating genetic, direct dating, and morphological dimensions simultaneously. Three of these skeletal fragments fit directly on Neandertal 1, whereas several others have distinctively Neandertal features. At least three individuals are represented in the skeletal sample. Radiocarbon dates for Neandertal 1, from which a mtDNA sequence was determined in 1997, and a second individual indicate an age of approximately 40,000 yr for both. mtDNA analysis on the same second individual yields a sequence that clusters with other published Neandertal sequences.