We reported several scientific discoveries, implicitly recognized by the commenters: Fronteira Oeste Rift; description of a unique, forgotten 15,000 km² area in Brazil that displays the contact of a large Cretaceous paleoerg with a large continental basaltic province; Catalán andesite covering most of the active erg; abundant evidence of hydrothermalism and vapor explosion from the Guarani Aquifer into and over overlying seal rocks; minor ergs not observed above the first lava flows; shape and structure of numerous barchan and seif paleodunes indicate more variable wind directions than previously reported. We used the methodology required to describe the processes. Cerro do Jarau is a compound paleodune (barchan and seif). We acknowledge the qualified comments made by the commenters, but our main evaluation remains unmodified. Continued studies will lead to significant contributions to the understanding of this major eolian-basaltic province in a unique relationship in the continents.

我们报道了几项科学发现，评论者含蓄地承认：Fronteira Oeste Rift；描述一个独特的、被遗忘的 15,000 公里²巴西的一个地区，显示了一个大型白垩纪古尔格与一个大型大陆玄武岩省的接触；加泰罗尼亚安山岩覆盖了大部分活跃的尔格；从瓜拉尼含水层进入和覆盖上覆密封岩的热液作用和蒸汽爆炸的大量证据；在第一次熔岩流上方未观察到较小的 ergs；许多新月形和赛义夫古丘的形状和结构表明比以前报道的风向变化更大。我们使用了描述过程所需的方法。Cerro do Jarau 是一个复合古丘（barchan 和 seif）。我们承认评论者提出的合格评论，但我们的主要评估仍未修改。继续研究将对理解这个主要风成玄武岩省在大陆上独特的关系做出重大贡献。