Abstract. Sediment-routing systems continuously transfer information and mass from eroding source areas to depositional sinks. Understanding how these systems alter environmental signals is critical when it comes to inferring source-area properties from the sedimentary record. We measure cosmogenic

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Response to Reviews Struck et al. -Tracking the 10Be-26Al source-area signal in sediment-routing systems of arid central AustraliaHere we respond to referee comments and provide explanations of our revisions. We thank the referees for their constructive and supportive suggestions. We have by and large followed them all. Referee comments are marked RC plus a sequential number. Our responses are marked R and keyed to page P and line L. Our response to all referee and short comments is also attached as a pdf document.Referee #1 (Comments to the author):RC1 -Cosmogenic isotopes, such as 10Be, have been used as tracers for sediment C1

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Here we respond to referee comments and provide explanations of our revisions. We thank the referees for their constructive and supportive suggestions. We have by and large followed them all. Referee comments are marked RC plus a sequential number. Our responses are marked R and keyed to page P and line L. Our response to all referee and short comments is also attached as a pdf document.Referee #2 (Comments to the author):RC5 -Line 4 of Abstract mentions "the factors responsible" but the authors do not say C1 ESurfDInteractive commentPrinter-friendly version Discussion paper