• Gn, Duda
• Liu, Y.
• Kerschnitzki, Michael
• Liu, Yifei
• Wagermaier, Wolfgang
• Fratzl, P.
• Duda, Georg N.
• Fratzl, Prof. Dr. Dr. H. C. Peter
• Kerschnitzki, M.
• Wagermaier, W.
• Roschger, Paul
• Roschger, P.

Abstract

The mechanical properties of bone are known to depend on its structure at all length scales. In large animals, such as sheep, cortical bone grows very quickly and it is known that this occurs in 2 stages whereby a poorly ordered (mostly woven) bone structure is initially deposited and later augmented and partially replaced by parallel fibered and lamellar bone with much improved mechanical properties, often called primary osteons. Most interestingly, a similar sequence of events has also recently been observed during callus formation in a sheep osteotomy model. This has prompted the idea that fast intramembranous bone formation requires an intermediate step where bone with a lower degree of collagen orientation is deposited first as a substrate for osteoblasts to coordinate the synthesis of lamellar tissue. Since some osteoblasts become embedded in the mineralizing collagen matrix which they synthesize, the resulting osteocyte network is a direct image of the location of osteoblasts during bone formation. Using 3-dimensional imaging of osteocyte networks as well as tissue characterization by polarized light microscopy and backscattered electron imaging, we revisit the structure of growing plexiform (fibrolamellar) bone and callus in sheep. We show that bone deposited initially is based on osteocytes without spatial correlation and encased in poorly ordered matrix. Bone deposited on top of this has lamellar collagen orientation as well as a layered arrangement of osteocytes, both parallel to the surfaces of the initial tissue. This supports the hypothesis that the initial bone constitutes an endogenous scaffold for the subsequent deposition of parallel fibered and lamellar bone.

Topics

• Deposition
• impedance spectroscopy
• surface
• layered
• woven
• Polarized light microscopy